Article(id=1309816805019975985, tenantId=1146029695717560320, journalId=1308397449582313577, issueId=1309816719896568193, articleNumber=null, orderNo=null, doi=10.7605/gdlxb.2026.106, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=research-article, receivedDate=1763740800000, receivedDateStr=2025-11-22, revisedDate=1768147200000, revisedDateStr=2026-01-12, acceptedDate=null, acceptedDateStr=null, onlineDate=1790214261535, onlineDateStr=2026-09-24, pubDate=1785513600000, pubDateStr=2026-08-01, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1790214261535, onlineIssueDateStr=2026-09-24, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1790214261535, creator=13701087609, updateTime=1790214261535, updator=13701087609, issue=Issue{id=1309816719896568193, tenantId=1146029695717560320, journalId=1308397449582313577, year='2026', volume='28', issue='4', pageStart='1217', pageEnd='1630', issueExtLink='null', onlineDate='null', pubDate='1785513600000', pubDateStr='2026-08-01', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=1, issueType=1, specialIssue=null, createTime=1790214241241, creator='13701087609', updateTime=1790214365545, updator='13701087609', preIssue=null, nextIssue=null, articleTotal=null, ext={EN=IssueExt(id=1309817241349223276, tenantId=1146029695717560320, journalId=1308397449582313577, issueId=1309816719896568193, language=EN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=), CN=IssueExt(id=1309817241349223277, tenantId=1146029695717560320, journalId=1308397449582313577, issueId=1309816719896568193, language=CN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=)}, issueFiles=null, downloadFileDto=null}, startPage=1461, endPage=1477, ext={EN=ArticleExt(id=1309816805489738034, articleId=1309816805019975985, tenantId=1146029695717560320, journalId=1308397449582313577, language=EN, title=Analysis of heavy mineral assemblages and clastic components in sandstones and their implications for provenance transport pathways: a case study of the Cretaceous Bashijiqike Formation in Keshen area,Kuqa Depression, columnId=1309816740377363171, journalTitle=Journal of Palaeogeography (Chinese Edition), columnName=PALAEOGEOGRAPHY, runingTitle=null, highlight=null, articleAbstract=
Due to intense tectonic compression,the massive sandstone of the Bashijiqike Formation in the Cretaceous within the piedmont belt of the Kuqa Depression exhibit severe deformation,complex seismic imaging,and high ambiguity,resulting in limited methods and even fewer achievements in the detailed study of provenance transport pathway in the Keshen natural gas accumulation area. In response to this issue,a comprehensive study was conducted on the heavy mineral assemblages of over 400 sandstone samples from more than 40 wells in the Bashijiqike Formation of the Keshen area,as well as experimental analyses including sandstone clastic components and cathodoluminescence on over 600 samples from 26 wells. The results show that: (1)Zircon,tourmaline,garnet,and magnetite are consistently present as heavy minerals in the wells of this area. The presence and variations in the content of stable heavy minerals such as rutile,apatite,and titanite,along with unstable heavy minerals like epidote,chlorite,and mica,lead to differences in heavy mineral assemblages across well zones. Combined with the ZTR index,these variations can help determine the differences in sedimentary provenance pathways among the well zones. (2)The sedimentary source rocks of the thick sandstone mainly come from pre Carboniferous high-grade metamorphic rocks,low-grade metamorphic rocks,intermediate acidic igneous rocks,basic igneous rocks,and sedimentary rocks,which can be subdivided into nine heavy mineral combination zones from east to west. (3)Due to the control of the content of sandstone debris components by primitive sedimentation,the planar variation characteristics of the average content of potassium feldspar,plagioclase,and metamorphic rock debris in sandstone debris components indicate the existence of 5-7 source transport pathways. (4)Based on a comprehensive analysis of the characteristics of source pathways indicated by heavy mineral assemblages and sandstone debris components,it is believed that there were at least seven source transport pathways from east to west during the sedimentation period of the Bashijiqike Formation,among which Zone Ⅱ and Zone Ⅴ may have been channels with longer river extensions. The above understanding provides a basis for the analysis of large-scale sedimentary microfacies and favorable sand body distribution in the Keshen area,supporting the fine research and evaluation of gas reservoirs in this area.
, authors=Zekun GUO
1, Zhiyong GAO
2, Xinluo FENG
1, Yijia LI
1, Kun ZHOU
1, Jianzhong LIU
1, Yu HE
2, Baizhi WANG
1, authorsList=Zekun GUO, Zhiyong GAO, Xinluo FENG, Yijia LI, Kun ZHOU, Jianzhong LIU, Yu HE, Baizhi WANG, authorCompany=null, correspAuthors=Zhiyong GAO, authorNote=
GUO Zekun,born in 1997,is a master’s degree holder and engineer. He is mainly engaged in development geology research work. E-mail: gzkun-tlm@petrochina.com.cn.
, correspAuthorsNote=
GAO Zhiyong,born in 1974,is a senior engineer. He is mainly engaged in sedimentology and reservoir geology,development geology. E-mail:
gzybox@163.com.
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*, columnId=1309816740561912549, journalTitle=古地理学报, columnName=古地理学, runingTitle=null, highlight=null, articleAbstract=
由于受强烈构造挤压作用,库车坳陷山前带白垩系巴什基奇克组巨厚砂岩变形强烈、地震成像复杂且多解性强,导致克深天然气富集区沉积物源通道精细研究的方法少、成果更少。针对此问题,开展了克深地区巴什基奇克组40余口钻井400多块砂岩样品的重矿物组合分析,26口钻井600余块样品的砂岩碎屑组分与阴极发光等实验分析,结果表明: (1)该区各井中锆石、电气石、石榴子石、磁铁矿等重矿物稳定存在,金红石、磷灰石、榍石等稳定重矿物与绿帘石、绿泥石、云母等不稳定重矿物是否存在及含量的差异导致各井区重矿物组合不同,辅以ZTR指数大小可判断各井区物源输送通道的差异; (2)巨厚砂岩的沉积物源母岩主要来自于前石炭系高级变质岩、低级变质岩、中酸性火成岩、基性火成岩与沉积岩,自东向西可细分为9个重矿物组合区; (3)由于砂岩碎屑组分的含量受原始沉积作用控制,砂岩碎屑组分中钾长石、斜长石及变质岩岩屑平均含量平面变化特征显示存在5~7个物源输送通道; (4)综合分析重矿物组合与砂岩碎屑组分分别指示的物源通道特征,认为巴什基奇克组沉积时期自东向西至少存在7条物源输送通道,其中Ⅱ区和Ⅴ区可能是河道延伸较远的通道。以上认识为克深地区大比例尺沉积微相及有利砂体展布分析提供依据,支撑了该区气藏精细研究与评价。
, authors=郭泽坤
1, 高志勇
2, 冯信荦
1, 李怡佳
1, 周坤
1, 刘剑忠
1, 何羽
2, 王柏智
1, authorsList=郭泽坤, 高志勇, 冯信荦, 李怡佳, 周坤, 刘剑忠, 何羽, 王柏智, authorCompany=null, correspAuthors=高志勇, authorNote=
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1 中国石油塔里木油田公司勘探开发研究院, 新疆库尔勒 841000, bio={"content":"
郭泽坤,男,1997年生,硕士,工程师,主要从事开发地质研究工作。E-mail: gzkun-tlm@petrochina.com.cn。
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郭泽坤,男,1997年生,硕士,工程师,主要从事开发地质研究工作。E-mail: gzkun-tlm@petrochina.com.cn。
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1 Research Institute of Petroleum Exploration and Development Center for Tarim Oilfield Company, PetroChina, Xinjiang Korla 841000, China, bio=null, bioImg=null, bioContent=null, aboutCorrespAuthor=null), CN=AuthorExt(id=1309816810371907934, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, authorId=1309816810216718683, language=CN, stringName=冯信荦, firstName=null, middleName=null, lastName=null, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=
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1 Research Institute of Petroleum Exploration and Development Center for Tarim Oilfield Company, PetroChina, Xinjiang Korla 841000, China, bio=null, bioImg=null, bioContent=null, aboutCorrespAuthor=null), CN=AuthorExt(id=1309816810627760483, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, authorId=1309816810439016800, language=CN, stringName=李怡佳, firstName=null, middleName=null, lastName=null, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=
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1 Research Institute of Petroleum Exploration and Development Center for Tarim Oilfield Company, PetroChina, Xinjiang Korla 841000, China, bio=null, bioImg=null, bioContent=null, aboutCorrespAuthor=null), CN=AuthorExt(id=1309816810841669992, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, authorId=1309816810694869349, language=CN, stringName=周坤, firstName=null, middleName=null, lastName=null, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=
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1 中国石油塔里木油田公司勘探开发研究院, 新疆库尔勒 841000, bio=null, bioImg=null, bioContent=null, aboutCorrespAuthor=null)}, companyList=[AuthorCompany(id=1309816809273000264, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, xref=1, ext=[AuthorCompanyExt(id=1309816809285583177, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, companyId=1309816809273000264, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=
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1 Research Institute of Petroleum Exploration and Development Center for Tarim Oilfield Company, PetroChina, Xinjiang Korla 841000, China, bio=null, bioImg=null, bioContent=null, aboutCorrespAuthor=null), CN=AuthorExt(id=1309816811214963053, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, authorId=1309816810938138986, language=CN, stringName=刘剑忠, firstName=null, middleName=null, lastName=null, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=
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2 Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, China, bio=null, bioImg=null, bioContent=null, aboutCorrespAuthor=null), CN=AuthorExt(id=1309816811462426994, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, authorId=1309816811277877615, language=CN, stringName=何羽, firstName=null, middleName=null, lastName=null, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=
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2 中国石油勘探开发研究院, 北京 100083, bio=null, bioImg=null, bioContent=null, aboutCorrespAuthor=null)}, companyList=[AuthorCompany(id=1309816809541435723, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, xref=2, ext=[AuthorCompanyExt(id=1309816809554018636, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, companyId=1309816809541435723, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=
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1 中国石油塔里木油田公司勘探开发研究院, 新疆库尔勒 841000, bio=null, bioImg=null, bioContent=null, aboutCorrespAuthor=null)}, companyList=[AuthorCompany(id=1309816809273000264, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, xref=1, ext=[AuthorCompanyExt(id=1309816809285583177, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, companyId=1309816809273000264, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=
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2012. 塔里木盆地库车坳陷白垩系巴什基奇克组物源精细分析.
天然气地球科学,
23(6): 1025-1033., articleTitle=塔里木盆地库车坳陷白垩系巴什基奇克组物源精细分析, refAbstract=null), Reference(id=1309816819075088805, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2012, volume=23, issue=6, pageStart=1025, pageEnd=1033, url=null, language=null, rfNumber=[1], rfOrder=1, authorNames=Chen G, Huang Z B, Zhang H L, Zhang R H, Yan X F, journalName=Natural Gas Geoscience, refType=null, unstructuredReference=[
Chen G,
Huang Z B,
Zhang H L,
Zhang R H,
Yan X F.
2012. Provenance analysis of clastic rocks in the Cretaceous Bashijiqike Formation at Kuqa Depression.
Natural Gas Geoscience,
23(6): 1025-1033], articleTitle=Provenance analysis of clastic rocks in the Cretaceous Bashijiqike Formation at Kuqa Depression, refAbstract=null), Reference(id=1309816819133809062, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2021, volume=26, issue=2, pageStart=77, pageEnd=84, url=null, language=null, rfNumber=[2], rfOrder=2, authorNames=程明, 刘永福, 刘运宏, 孙琦, 周思宇, 蒋俊, journalName=中国石油勘探, refType=null, unstructuredReference=程明, 刘永福, 刘运宏, 孙琦, 周思宇, 蒋俊.
2021. 塔里木盆地羊塔11井区白垩系亚格列木组物源分析.
中国石油勘探,
26(2): 77-84., articleTitle=塔里木盆地羊塔11井区白垩系亚格列木组物源分析, refAbstract=null), Reference(id=1309816819196723623, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2021, volume=26, issue=2, pageStart=77, pageEnd=84, url=null, language=null, rfNumber=[2], rfOrder=3, authorNames=Cheng M, Liu Y F, Liu Y H, Sun Q, Zhou S Y, Jiang J, journalName=China Petroleum Exploration, refType=null, unstructuredReference=[
Cheng M,
Liu Y F,
Liu Y H,
Sun Q,
Zhou S Y,
Jiang J.
2021. Provenance analysis of Cretaceous Yageliemu Formation in the Yangta 11 well block,Tarim Basin.
China Petroleum Exploration,
26(2): 77-84], articleTitle=Provenance analysis of Cretaceous Yageliemu Formation in the Yangta 11 well block,Tarim Basin, refAbstract=null), Reference(id=1309816819276415400, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2017, volume=24, issue=1, pageStart=70, pageEnd=75, url=null, language=null, rfNumber=[3], rfOrder=4, authorNames=冯洁, 宋岩, 姜振学, 李宝帅, 李峰, journalName=特种油气藏, refType=null, unstructuredReference=冯洁, 宋岩, 姜振学, 李宝帅, 李峰.
2017. 塔里木盆地克深区巴什基奇克组砂岩成岩演化及主控因素.
特种油气藏,
24(1): 70-75., articleTitle=塔里木盆地克深区巴什基奇克组砂岩成岩演化及主控因素, refAbstract=null), Reference(id=1309816819347718569, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2017, volume=24, issue=1, pageStart=70, pageEnd=75, url=null, language=null, rfNumber=[3], rfOrder=5, authorNames=Feng J, Song Y, Jiang Z X, Li B S, Li F, journalName=Special Oil and Gas Reservoirs, refType=null, unstructuredReference=[
Feng J,
Song Y,
Jiang Z X,
Li B S,
Li F.
2017. Diagenetic evolution and major controlling factors for sandstone in Bashijiqike Formation of the Keshen Area in the Tarim Basin.
Special Oil and Gas Reservoirs,
24(1): 70-75], articleTitle=Diagenetic evolution and major controlling factors for sandstone in Bashijiqike Formation of the Keshen Area in the Tarim Basin, refAbstract=null), Reference(id=1309816819620348330, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2014, volume=32, issue=6, pageStart=1060, pageEnd=1071, url=null, language=null, rfNumber=[4], rfOrder=6, authorNames=高志勇, 冯佳睿, 周川闽, 崔京钢, 李小陪, 赵雪松, 郭美丽, 吴昊, journalName=沉积学报, refType=null, unstructuredReference=高志勇, 冯佳睿, 周川闽, 崔京钢, 李小陪, 赵雪松, 郭美丽, 吴昊.
2014. 干旱气候环境下季节性河流沉积特征: 以库车河剖面下白垩统为例.
沉积学报,
32(6): 1060-1071., articleTitle=干旱气候环境下季节性河流沉积特征: 以库车河剖面下白垩统为例, refAbstract=null), Reference(id=1309816819712623019, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2014, volume=32, issue=6, pageStart=1060, pageEnd=1071, url=null, language=null, rfNumber=[4], rfOrder=7, authorNames=Gao Z Y, Feng J R, Zhou C M, Cui J G, Li X P, Zhao X S, Guo M L, Wu H, journalName=Acta Sedimentologica Sinica, refType=null, unstructuredReference=[
Gao Z Y,
Feng J R,
Zhou C M,
Cui J G,
Li X P,
Zhao X S,
Guo M L,
Wu H.
2014. Arid climateseasonal rivers deposition: a case of Lower Cretaceous in Kuche river outcrop.
Acta Sedimentologica Sinica,
32(6): 1060-1071], articleTitle=Arid climateseasonal rivers deposition: a case of Lower Cretaceous in Kuche river outcrop, refAbstract=null), Reference(id=1309816819796509100, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2016a, volume=34, issue=3, pageStart=415, pageEnd=435, url=null, language=null, rfNumber=[5], rfOrder=8, authorNames=高志勇, 周川闽, 冯佳睿, 吴昊, 李雯, journalName=沉积学报, refType=null, unstructuredReference=高志勇, 周川闽, 冯佳睿, 吴昊, 李雯.
2016a. 中新生代天山隆升及其南北盆地分异与沉积环境演化.
沉积学报,
34(3): 415-435., articleTitle=中新生代天山隆升及其南北盆地分异与沉积环境演化, refAbstract=null), Reference(id=1309816819888783790, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2016a, volume=34, issue=3, pageStart=415, pageEnd=435, url=null, language=null, rfNumber=[5], rfOrder=9, authorNames=Gao Z Y, Zhou C M, Feng J R, Wu H, Li W, journalName=Acta Sedimentologica Sinica, refType=null, unstructuredReference=[
Gao Z Y,
Zhou C M,
Feng J R,
Wu H,
Li W.
2016a. Relationship between the Tianshan mountains uplift and depositional environment evolution of the basins in Mesozoic-Cenozoic.
Acta Sedimentologica Sinica,
34(3): 415-435], articleTitle=Relationship between the Tianshan mountains uplift and depositional environment evolution of the basins in Mesozoic-Cenozoic, refAbstract=null), Reference(id=1309816820031390127, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2016b, volume=37, issue=8, pageStart=996, pageEnd=1010, url=null, language=null, rfNumber=[6], rfOrder=10, authorNames=高志勇, 周川闽, 冯佳睿, 吴昊, 李雯, journalName=石油学报, refType=null, unstructuredReference=高志勇, 周川闽, 冯佳睿, 吴昊, 李雯.
2016b. 库车坳陷白垩系巴什基奇克组泥砾的成因机制与厚层状砂体展布.
石油学报,
37(8): 996-1010., articleTitle=库车坳陷白垩系巴什基奇克组泥砾的成因机制与厚层状砂体展布, refAbstract=null), Reference(id=1309816820132053424, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2016b, volume=37, issue=8, pageStart=996, pageEnd=1010, url=null, language=null, rfNumber=[6], rfOrder=11, authorNames=Gao Z Y, Zhou C M, Feng J R, Wu H, Li W, journalName=Acta Petrolei Sinica, refType=null, unstructuredReference=[
Gao Z Y,
Zhou C M,
Feng J R,
Wu H,
Li W.
2016b. Mechanism and sedimentary environment of the muddy gravel concomitant with thick layer sandstone of Cretaceous in Kuqa Depression.
Acta Petrolei Sinica,
37(8): 996-1010], articleTitle=Mechanism and sedimentary environment of the muddy gravel concomitant with thick layer sandstone of Cretaceous in Kuqa Depression, refAbstract=null), Reference(id=1309816820199162289, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2019, volume=null, issue=null, pageStart=1, pageEnd=12, url=null, language=null, rfNumber=[7], rfOrder=12, authorNames=高志勇, 张锡新, 张东峰, 贺银军, 郭鹏超, 南珺祥, 高波, 方正伟, 谢巍, 张磊, 黄向剩, 臧春艳, 宋梅芳, 柳娜, journalName=null, refType=null, unstructuredReference=高志勇, 张锡新, 张东峰, 贺银军, 郭鹏超, 南珺祥, 高波, 方正伟, 谢巍, 张磊, 黄向剩, 臧春艳, 宋梅芳, 柳娜.
2019. 石油与天然气行业标准《沉积岩重矿物分离与鉴定方法》SY/T 6336-2019, 1-12., articleTitle=石油与天然气行业标准《沉积岩重矿物分离与鉴定方法》SY/T 6336-2019, refAbstract=null), Reference(id=1309816820442431922, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2019, volume=null, issue=null, pageStart=1, pageEnd=12, url=null, language=null, rfNumber=[7], rfOrder=13, authorNames=Gao Z Y, Zhang X X, Zhang D F, He Y J, Guo P C, Nan J X, Gao B, Fang Z W, Xie W, Zhang L, Huang X S, Zang C Y, Song M F, Liu N, journalName=null, refType=null, unstructuredReference=[
Gao Z Y,
Zhang X X,
Zhang D F,
He Y J,
Guo P C,
Nan J X,
Gao B,
Fang Z W,
Xie W,
Zhang L,
Huang X S,
Zang C Y,
Song M F,
Liu N.
2019. The method of separation and examination of heavey minerals for sedimentary rock: SY/T 6336-2919, 1-12], articleTitle=The method of separation and examination of heavey minerals for sedimentary rock: SY/T 6336-2919, refAbstract=null), Reference(id=1309816820530512307, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2021, volume=95, issue=12, pageStart=3606, pageEnd=3628, url=null, language=null, rfNumber=[8], rfOrder=14, authorNames=高志勇, 王华建, 冯佳睿, 罗忠, 张宇航, 李晓红, journalName=地质学报, refType=null, unstructuredReference=高志勇, 王华建, 冯佳睿, 罗忠, 张宇航, 李晓红.
2021. 燕辽海盆中元古界下马岭组沉积期的物源性质与古地理环境.
地质学报,
95(12): 3606-3628., articleTitle=燕辽海盆中元古界下马岭组沉积期的物源性质与古地理环境, refAbstract=null), Reference(id=1309816820593426868, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2021, volume=95, issue=12, pageStart=3606, pageEnd=3628, url=null, language=null, rfNumber=[8], rfOrder=15, authorNames=Gao Z Y, Wang H J, Feng J R, Luo Z, Zhang Y H, Li X H, journalName=Acta Geologica Sinica, refType=null, unstructuredReference=[
Gao Z Y,
Wang H J,
Feng J R,
Luo Z,
Zhang Y H,
Li X H.
2021. Provenance and paleogeographic environment of the Middle Proterozoic Xiamaling Formation in the Yanliao Basin.
Acta Geologica Sinica,
95(12): 3606-3628], articleTitle=Provenance and paleogeographic environment of the Middle Proterozoic Xiamaling Formation in the Yanliao Basin, refAbstract=null), Reference(id=1309816820660535733, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2020, volume=45, issue=6, pageStart=2186, pageEnd=2198, url=null, language=null, rfNumber=[9], rfOrder=16, authorNames=何杰, 王华, Eduardo Garzanti, journalName=地球科学, refType=null, unstructuredReference=何杰, 王华, Eduardo Garzanti.
2020. 砂岩(砂)的岩相分析和分类标准.
地球科学,
45(6): 2186-2198., articleTitle=砂岩(砂)的岩相分析和分类标准, refAbstract=null), Reference(id=1309816820723450294, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2020, volume=45, issue=6, pageStart=2186, pageEnd=2198, url=null, language=null, rfNumber=[9], rfOrder=17, authorNames=He J, Wang H, Eduardo G, journalName=Earth Science, refType=null, unstructuredReference=[
He J,
Wang H,
Eduardo G.
2020. Petrographic analysis and classification of sand and sandstone.
Earth Science,
45(6): 2186-2198], articleTitle=Petrographic analysis and classification of sand and sandstone, refAbstract=null), Reference(id=1309816820786364855, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2000, volume=7, issue=3, pageStart=133, pageEnd=143, url=null, language=null, rfNumber=[10], rfOrder=18, authorNames=贾进华, journalName=地学前缘, refType=null, unstructuredReference=贾进华.
2000. 库车前陆盆地白垩纪巴什基奇克组沉积层序与储层研究.
地学前缘,
7(3): 133-143., articleTitle=库车前陆盆地白垩纪巴什基奇克组沉积层序与储层研究, refAbstract=null), Reference(id=1309816820945748408, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2000, volume=7, issue=3, pageStart=133, pageEnd=143, url=null, language=null, rfNumber=[10], rfOrder=19, authorNames=Jia J H, journalName=Earth Sciences Frontiers, refType=null, unstructuredReference=[
Jia J H.
2000. Depositional sequence and reservoir of Cretaceous Bashijiqike Formation in Kuqa foreland basin.
Earth Sciences Frontiers,
7(3): 133-143], articleTitle=Depositional sequence and reservoir of Cretaceous Bashijiqike Formation in Kuqa foreland basin, refAbstract=null), Reference(id=1309816821012857273, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2012, volume=27, issue=8, pageStart=828, pageEnd=846, url=null, language=null, rfNumber=[11], rfOrder=20, authorNames=简星, 关平, 张巍, journalName=地球科学进展, refType=null, unstructuredReference=简星, 关平, 张巍.
2012. 碎屑金红石: 沉积物源的一种指针.
地球科学进展,
27(8): 828-846., articleTitle=碎屑金红石: 沉积物源的一种指针, refAbstract=null), Reference(id=1309816821302264250, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2012, volume=27, issue=8, pageStart=828, pageEnd=846, url=null, language=null, rfNumber=[11], rfOrder=21, authorNames=Jian X, Guan P, Zhang W, journalName=Advances in Earth Science, refType=null, unstructuredReference=[
Jian X,
Guan P,
Zhang W.
2012. Detrital rutile: a sediment provenance indicator.
Advances in Earth Science,
27(8): 828-846], articleTitle=Detrital rutile: a sediment provenance indicator, refAbstract=null), Reference(id=1309816821394538939, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2006a, volume=41, issue=3, pageStart=465, pageEnd=478, url=null, language=null, rfNumber=[12], rfOrder=22, authorNames=李双建, 王清晨, 李忠, 王道轩, journalName=地质科学, refType=null, unstructuredReference=李双建, 王清晨, 李忠, 王道轩.
2006a. 砂岩碎屑组份变化对库车坳陷和南天山盆山演化的指示.
地质科学,
41(3): 465-478., articleTitle=砂岩碎屑组份变化对库车坳陷和南天山盆山演化的指示, refAbstract=null), Reference(id=1309816821478425020, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2006a, volume=41, issue=3, pageStart=465, pageEnd=478, url=null, language=null, rfNumber=[12], rfOrder=23, authorNames=Li S J, Wang Q C, Li Z, Wang D X, journalName=Chinese Journal of Geology, refType=null, unstructuredReference=[
Li S J,
Wang Q C,
Li Z,
Wang D X.
2006a. Detrital modes sandstones and their implications for basin-mountain evolution between the Kuqa depression and south Tian Shan Mountains.
Chinese Journal of Geology,
41(3): 465-478], articleTitle=Detrital modes sandstones and their implications for basin-mountain evolution between the Kuqa depression and south Tian Shan Mountains, refAbstract=null), Reference(id=1309816821717500349, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2006b, volume=24, issue=1, pageStart=28, pageEnd=35, url=null, language=null, rfNumber=[13], rfOrder=24, authorNames=李双建, 石永红, 王清晨, journalName=沉积学报, refType=null, unstructuredReference=李双建, 石永红, 王清晨.
2006b. 碎屑重矿物分析对库车坳陷白垩—第三纪物源变化的指示.
沉积学报,
24(1): 28-35., articleTitle=碎屑重矿物分析对库车坳陷白垩—第三纪物源变化的指示, refAbstract=null), Reference(id=1309816821792997822, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2006b, volume=24, issue=1, pageStart=28, pageEnd=35, url=null, language=null, rfNumber=[13], rfOrder=25, authorNames=Li S J, Shi Y H, Wang Q C, journalName=Acta Sedimentologica Sinica, refType=null, unstructuredReference=[
Li S J,
Shi Y H,
Wang Q C.
2006b. The analysis of detrital heavy minerals in Cretaceous-Tertiary sandstones,Kuqa depression and their implications for provenance.
Acta Sedimentologica Sinica,
24(1): 28-35], articleTitle=The analysis of detrital heavy minerals in Cretaceous-Tertiary sandstones,Kuqa depression and their implications for provenance, refAbstract=null), Reference(id=1309816821864300991, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2007, volume=42, issue=4, pageStart=709, pageEnd=721, url=null, language=null, rfNumber=[14], rfOrder=26, authorNames=李双建, 石永红, 王清晨, 李忠, journalName=地质科学, refType=null, unstructuredReference=李双建, 石永红, 王清晨, 李忠.
2007. 白垩纪以来库车坳陷碎屑重矿物组成变化.
地质科学,
42(4): 709-721., articleTitle=白垩纪以来库车坳陷碎屑重矿物组成变化, refAbstract=null), Reference(id=1309816821935604160, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2007, volume=42, issue=4, pageStart=709, pageEnd=721, url=null, language=null, rfNumber=[14], rfOrder=27, authorNames=Li S J, Shi Y H, Wang Q C, Li Z, journalName=Chinese Journal of Geology, refType=null, unstructuredReference=[
Li S J,
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Li Z.
2007. Changes of detrital heavey minerals’ composition in the Kuqa depression from Cretaceous.
Chinese Journal of Geology,
42(4): 709-721], articleTitle=Changes of detrital heavey minerals’ composition in the Kuqa depression from Cretaceous, refAbstract=null), Reference(id=1309816822141125057, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2014, volume=88, issue=2, pageStart=167, pageEnd=184, url=null, language=null, rfNumber=[15], rfOrder=28, authorNames=李双应, 杨栋栋, 王松, 万秋, 王道轩, journalName=地质学报, refType=null, unstructuredReference=李双应, 杨栋栋, 王松, 万秋, 王道轩.
2014. 南天山中段上石炭统碎屑岩岩石学、地球化学、重矿物和锆石年代学特征及其对物源区、构造演化的约束.
地质学报,
88(2): 167-184., articleTitle=南天山中段上石炭统碎屑岩岩石学、地球化学、重矿物和锆石年代学特征及其对物源区、构造演化的约束, refAbstract=null), Reference(id=1309816822208233922, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2014, volume=88, issue=2, pageStart=167, pageEnd=184, url=null, language=null, rfNumber=[15], rfOrder=29, authorNames=Li S Y, Yang D D, Wang S, Wan Q, Wang D X, journalName=Acta Geologica Sinica, refType=null, unstructuredReference=[
Li S Y,
Yang D D,
Wang S,
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2014. Characteristics of petrology,geochemistry,heavey minerals and isotope chronology of Upper Carboniferous detrital rocks in the middle segment of South Tianshan and constraints to the provenance and tectonic evolution.
Acta Geologica Sinica,
88(2): 167-184], articleTitle=Characteristics of petrology,geochemistry,heavey minerals and isotope chronology of Upper Carboniferous detrital rocks in the middle segment of South Tianshan and constraints to the provenance and tectonic evolution, refAbstract=null), Reference(id=1309816822292120004, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2004, volume=20, issue=3, pageStart=655, pageEnd=666, url=null, language=null, rfNumber=[16], rfOrder=30, authorNames=李忠, 王道轩, 林伟, 王清晨, journalName=岩石学报, refType=null, unstructuredReference=李忠, 王道轩, 林伟, 王清晨.
2004. 库车坳陷中—新生界碎屑组分对物源类型及其构造属性的指示.
岩石学报,
20(3): 655-666., articleTitle=库车坳陷中—新生界碎屑组分对物源类型及其构造属性的指示, refAbstract=null), Reference(id=1309816822371811781, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2004, volume=20, issue=3, pageStart=655, pageEnd=666, url=null, language=null, rfNumber=[16], rfOrder=31, authorNames=Li Z, Wang D X, Lin W, Wang Q C, journalName=Acta Petrologica Sinica, refType=null, unstructuredReference=[
Li Z,
Wang D X,
Lin W,
Wang Q C.
2004. Mesozoic-Cenozoic clastic composition in Kuqa Depression,northwest China: implication for provenance types and tectonic attributes.
Acta Petrologica Sinica,
20(3): 655-666], articleTitle=Mesozoic-Cenozoic clastic composition in Kuqa Depression,northwest China: implication for provenance types and tectonic attributes, refAbstract=null), Reference(id=1309816822594109894, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2025, volume=27, issue=4, pageStart=870, pageEnd=885, url=null, language=null, rfNumber=[17], rfOrder=32, authorNames=黎立, 孙春燕, 董尧, 罗强, 屈洋, 朱世发, journalName=古地理学报, refType=null, unstructuredReference=黎立, 孙春燕, 董尧, 罗强, 屈洋, 朱世发.
2025. 塔西南山前地区甫沙断陷侏罗系物源与沉积相.
古地理学报,
27(4): 870-885., articleTitle=塔西南山前地区甫沙断陷侏罗系物源与沉积相, refAbstract=null), Reference(id=1309816822677995975, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2025, volume=27, issue=4, pageStart=870, pageEnd=885, url=null, language=null, rfNumber=[17], rfOrder=33, authorNames=Li L, Sun C Y, Dong Y, Luo Q, Qu Y, Zhu S F, journalName=Journal of Palaeogeography(Chinese Edition), refType=null, unstructuredReference=[
Li L,
Sun C Y,
Dong Y,
Luo Q,
Qu Y,
Zhu S F.
2025. Provenance and sedimentary facies of the Jurassic in Fusha fault depression,piedmont area of southwestern Tarim Basin.
Journal of Palaeogeography(Chinese Edition),
27(4): 870-885], articleTitle=Provenance and sedimentary facies of the Jurassic in Fusha fault depression,piedmont area of southwestern Tarim Basin, refAbstract=null), Reference(id=1309816822749299144, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2007, volume=26, issue=6, pageStart=10, pageEnd=16, url=null, language=null, rfNumber=[18], rfOrder=34, authorNames=刘嵘, 董月霞, 谭靖, 张素新, journalName=地质科技情报, refType=null, unstructuredReference=刘嵘, 董月霞, 谭靖, 张素新.
2007. 沉积岩中稳定重砂矿物的成岩蚀变特征及其指示意义.
地质科技情报,
26(6): 10-16., articleTitle=沉积岩中稳定重砂矿物的成岩蚀变特征及其指示意义, refAbstract=null), Reference(id=1309816822816408009, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2007, volume=26, issue=6, pageStart=10, pageEnd=16, url=null, language=null, rfNumber=[18], rfOrder=35, authorNames=Liu R, Dong Y X, Tan J, Zhang S X, journalName=Geological Science and Technology Information, refType=null, unstructuredReference=[
Liu R,
Dong Y X,
Tan J,
Zhang S X.
2007. Diagenesis alteration of heavy minerals of garnet,zircon,rutile,apatite,tourmaline and titanite during diagenesis and its geological significance.
Geological Science and Technology Information,
26(6): 10-16], articleTitle=Diagenesis alteration of heavy minerals of garnet,zircon,rutile,apatite,tourmaline and titanite during diagenesis and its geological significance, refAbstract=null), Reference(id=1309816822883516874, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2014, volume=30, issue=2, pageStart=597, pageEnd=608, url=null, language=null, rfNumber=[19], rfOrder=36, authorNames=马收先, 孟庆任, 曲永强, journalName=岩石学报, refType=null, unstructuredReference=马收先, 孟庆任, 曲永强.
2014. 轻矿物物源分析研究进展.
岩石学报,
30(2): 597-608., articleTitle=轻矿物物源分析研究进展, refAbstract=null), Reference(id=1309816823021928907, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2014, volume=30, issue=2, pageStart=597, pageEnd=608, url=null, language=null, rfNumber=[19], rfOrder=37, authorNames=Ma S X, Meng Q R, Qu Y Q, journalName=Acta Petrologica Sinica, refType=null, unstructuredReference=[
Ma S X,
Meng Q R,
Qu Y Q.
2014. Development on provenance analysis of light minerals.
Acta Petrologica Sinica,
30(2): 597-608], articleTitle=Development on provenance analysis of light minerals, refAbstract=null), Reference(id=1309816823089037772, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2025, volume=30, issue=2, pageStart=167, pageEnd=176, url=null, language=null, rfNumber=[20], rfOrder=38, authorNames=莫涛, 王珂, 王俊鹏, 金文正, journalName=海相油气地质, refType=null, unstructuredReference=莫涛, 王珂, 王俊鹏, 金文正.
2025. 库车坳陷白垩系沉积前古地貌及对沉积的控制作用.
海相油气地质,
30(2): 167-176., articleTitle=库车坳陷白垩系沉积前古地貌及对沉积的控制作用, refAbstract=null), Reference(id=1309816823156146637, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2025, volume=30, issue=2, pageStart=167, pageEnd=176, url=null, language=null, rfNumber=[20], rfOrder=39, authorNames=Mo T, Wang K, Wang J P, Jin W Z, journalName=Marine Origin Petroleum Geology, refType=null, unstructuredReference=[
Mo T,
Wang K,
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Jin W Z.
2025. Pre-Cretaceous paleogeomorphology and its control effect on sedimentation in Kuqa Depression.
Marine Origin Petroleum Geology,
30(2): 167-176], articleTitle=Pre-Cretaceous paleogeomorphology and its control effect on sedimentation in Kuqa Depression, refAbstract=null), Reference(id=1309816823219061198, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2020, volume=31, issue=8, pageStart=1126, pageEnd=1138, url=null, language=null, rfNumber=[21], rfOrder=40, authorNames=史超群, 张慧芳, 周思宇, 王佐涛, 蒋俊, 章学岐, 左小军, 娄洪, 王振鸿, 陈常超, journalName=天然气地球科学, refType=null, unstructuredReference=史超群, 张慧芳, 周思宇, 王佐涛, 蒋俊, 章学岐, 左小军, 娄洪, 王振鸿, 陈常超.
2020. 塔里木盆地库车坳陷克拉苏构造带—秋里塔格构造带白垩系巴什基奇克组深层、高产储层特征及控制因素.
天然气地球科学,
31(8): 1126-1138., articleTitle=塔里木盆地库车坳陷克拉苏构造带—秋里塔格构造带白垩系巴什基奇克组深层、高产储层特征及控制因素, refAbstract=null), Reference(id=1309816823290364367, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2020, volume=31, issue=8, pageStart=1126, pageEnd=1138, url=null, language=null, rfNumber=[21], rfOrder=41, authorNames=Shi C Q, Zhang H F, Zhou S Y, Wang Z T, Jiang J, Zhang X Q, Zuo X J, Lou H, Wang Z H, Chen C C, journalName=Natural Gas Geoscience, refType=null, unstructuredReference=[
Shi C Q,
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Zhou S Y,
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Jiang J,
Zhang X Q,
Zuo X J,
Lou H,
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2020. Comparative study on deep and high yielding reservoir characteristics and controlling factors of Cretaceous Bashijiqike Formation in Kelasu structural belt and Qiulitage structural belt of Kuqa Depression,Tarim Basin.
Natural Gas Geoscience,
31(8): 1126-1138], articleTitle=Comparative study on deep and high yielding reservoir characteristics and controlling factors of Cretaceous Bashijiqike Formation in Kelasu structural belt and Qiulitage structural belt of Kuqa Depression,Tarim Basin, refAbstract=null), Reference(id=1309816823370056144, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2015, volume=33, issue=4, pageStart=61, pageEnd=69, url=null, language=null, rfNumber=[22], rfOrder=42, authorNames=舒雨婷, 郑玉龙, 许冬, 初凤友, journalName=海洋学研究, refType=null, unstructuredReference=舒雨婷, 郑玉龙, 许冬, 初凤友.
2015. 西菲律宾海盆I8孔黏土矿物的物源分析.
海洋学研究,
33(4): 61-69., articleTitle=西菲律宾海盆I8孔黏土矿物的物源分析, refAbstract=null), Reference(id=1309816823441359313, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2015, volume=33, issue=4, pageStart=61, pageEnd=69, url=null, language=null, rfNumber=[22], rfOrder=43, authorNames=Shu Y T, Zheng Y L, Xu D, Chu F Y, journalName=Journal of Marine Sciences, refType=null, unstructuredReference=[
Shu Y T,
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2015. The provenance of chayminerals in core Ⅰ8 from the west Philippine Basin.
Journal of Marine Sciences,
33(4): 61-69], articleTitle=The provenance of chayminerals in core Ⅰ8 from the west Philippine Basin, refAbstract=null), Reference(id=1309816823512662482, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2018, volume=48, issue=3, pageStart=693, pageEnd=704, url=null, language=null, rfNumber=[23], rfOrder=44, authorNames=孙海涛, 钟大康, 李勇, 毛亚昆, 杨宪彰, journalName=吉林大学学报(地球科学版), refType=null, unstructuredReference=孙海涛, 钟大康, 李勇, 毛亚昆, 杨宪彰.
2018. 超深低孔特低渗砂岩储层的孔隙成因及控制因素: 以库车坳陷克深地区巴什基奇克组为例.
吉林大学学报(地球科学版),
48(3): 693-704., articleTitle=超深低孔特低渗砂岩储层的孔隙成因及控制因素: 以库车坳陷克深地区巴什基奇克组为例, refAbstract=null), Reference(id=1309816823579771347, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2018, volume=48, issue=3, pageStart=693, pageEnd=704, url=null, language=null, rfNumber=[23], rfOrder=45, authorNames=Sun H T, Zhong D K, Li Y, Mao Y K, Yang X Z, journalName=Journal of Jilin Univerity(Earth Science Edition), refType=null, unstructuredReference=[
Sun H T,
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2018. Porosity origin and controlling factors of ultra-deep,low porosity and ultral-low permeability sandstone reservoirs: a case study of Bashijiqike formation in Keshen area of Kuqa Depression,Tarim Basin.
Journal of Jilin Univerity(Earth Science Edition),
48(3): 693-704], articleTitle=Porosity origin and controlling factors of ultra-deep,low porosity and ultral-low permeability sandstone reservoirs: a case study of Bashijiqike formation in Keshen area of Kuqa Depression,Tarim Basin, refAbstract=null), Reference(id=1309816823659463124, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2018, volume=37, issue=5, pageStart=70, pageEnd=77, url=null, language=null, rfNumber=[24], rfOrder=46, authorNames=王翠丽, 李红波, 陈东, 陈宝新, 刘磊, 罗明高, journalName=地质科技情报, refType=null, unstructuredReference=王翠丽, 李红波, 陈东, 陈宝新, 刘磊, 罗明高.
2018. 克深气田巴什基奇克组致密砂岩储层孔隙结构特征及影响因素分析.
地质科技情报,
37(5): 70-77., articleTitle=克深气田巴什基奇克组致密砂岩储层孔隙结构特征及影响因素分析, refAbstract=null), Reference(id=1309816823734960597, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2018, volume=37, issue=5, pageStart=70, pageEnd=77, url=null, language=null, rfNumber=[24], rfOrder=47, authorNames=Wang C L, Li H B, Chen D, Chen B X, Liu L, Luo M G, journalName=Geological Science and Technology Information, refType=null, unstructuredReference=[
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2018. Porosity structure characteristics and influencing factors analysis of Bashijiqike tight sandstone reservoir in Keshen Gasfield.
Geological Science and Technology Information,
37(5): 70-77], articleTitle=Porosity structure characteristics and influencing factors analysis of Bashijiqike tight sandstone reservoir in Keshen Gasfield, refAbstract=null), Reference(id=1309816823877566934, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2021, volume=42, issue=2, pageStart=338, pageEnd=353, url=null, language=null, rfNumber=[25], rfOrder=48, authorNames=王珂, 张荣虎, 王俊鹏, 孙雄伟, 杨学君, journalName=石油与天然气地质, refType=null, unstructuredReference=王珂, 张荣虎, 王俊鹏, 孙雄伟, 杨学君.
2021. 超深层致密砂岩储层构造裂缝分布特征及其成因: 以塔里木盆地库车前陆冲断带克深气田为例.
石油与天然气地质,
42(2): 338-353., articleTitle=超深层致密砂岩储层构造裂缝分布特征及其成因: 以塔里木盆地库车前陆冲断带克深气田为例, refAbstract=null), Reference(id=1309816824238277079, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2021, volume=42, issue=2, pageStart=338, pageEnd=353, url=null, language=null, rfNumber=[25], rfOrder=49, authorNames=Wang K, Zhang R H, Wang J P, Sun X W, Yang X J, journalName=Oil & Gas Geology, refType=null, unstructuredReference=[
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2021. Distribution and origin of tectonic fractures in ultra-deep tight sandstone reservoirs: a case study of Keshen gas field,Kuqa foreland thrust belt,Tarim Basin.
Oil & Gas Geology,
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2014. 塔里木盆地库车坳陷克拉苏盐下深层大气田形成机制与富集规律.
天然气地球科学,
25(2): 153-166., articleTitle=塔里木盆地库车坳陷克拉苏盐下深层大气田形成机制与富集规律, refAbstract=null), Reference(id=1309816824657707481, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2014, volume=25, issue=2, pageStart=153, pageEnd=166, url=null, language=null, rfNumber=[26], rfOrder=51, authorNames=Wang Z M, journalName=Natural Gas Geoscience, refType=null, unstructuredReference=[
Wang Z M.
2014. Formation mechanism and enrichment regularities of Kelasu subsalt deep large gas field in Kuqa Depression,Tarim Basin.
Natural Gas Geoscience,
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2019. 碎屑岩物源研究进展与展望.
古地理学报,
21(3): 379-396., articleTitle=碎屑岩物源研究进展与展望, refAbstract=null), Reference(id=1309816825077137883, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2019, volume=21, issue=3, pageStart=379, pageEnd=396, url=null, language=null, rfNumber=[27], rfOrder=53, authorNames=Xu J, Jiang Z X, journalName=Journal of Palaeogeography(Chinese Edition), refType=null, unstructuredReference=[
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2019. Provenance analysis of clastic rocks: current research status and prospect.
Journal of Palaeogeography(Chinese Edition),
21(3): 379-396], articleTitle=Provenance analysis of clastic rocks: current research status and prospect, refAbstract=null), Reference(id=1309816825177801180, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2020, volume=42, issue=2, pageStart=172, pageEnd=187, url=null, language=null, rfNumber=[28], rfOrder=54, authorNames=许兴斌, 王昌勇, 刘满仓, 林世国, 李德江, 高志勇, journalName=地球科学与环境学报, refType=null, unstructuredReference=许兴斌, 王昌勇, 刘满仓, 林世国, 李德江, 高志勇.
2020. 塔里木盆地库车坳陷东部上三叠统—中侏罗统物源特征及其地质意义.
地球科学与环境学报,
42(2): 172-187., articleTitle=塔里木盆地库车坳陷东部上三叠统—中侏罗统物源特征及其地质意义, refAbstract=null), Reference(id=1309816825278464477, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2020, volume=42, issue=2, pageStart=172, pageEnd=187, url=null, language=null, rfNumber=[28], rfOrder=55, authorNames=Xu X B, Wang C Y, Liu M C, Lin S G, Li D J, Gao Z Y, journalName=Journal of Earth Sciences and Environment, refType=null, unstructuredReference=[
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2020. Provenance characteristics of Upper Triassic-Middle Jurassic in the eastern Kuqa depression of Tarim Basin,China.
Journal of Earth Sciences and Environment,
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2021. 塔里木盆地克深气田成藏条件及勘探开发关键技术.
石油学报,
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2021. Acumulation conditions,key exploration and development technologies for Keshen gas field in Tarim Basin.
Acta Petrolei Sinica,
42(3): 399-414], articleTitle=Acumulation conditions,key exploration and development technologies for Keshen gas field in Tarim Basin, refAbstract=null), Reference(id=1309816825974718945, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2013, volume=31, issue=1, pageStart=99, pageEnd=107, url=null, language=null, rfNumber=[30], rfOrder=58, authorNames=杨仁超, 李进步, 樊爱萍, 宗敏, 张涛, journalName=沉积学报, refType=null, unstructuredReference=杨仁超, 李进步, 樊爱萍, 宗敏, 张涛.
2013. 陆源沉积岩物源分析研究进展与发展趋势.
沉积学报,
31(1): 99-107., articleTitle=陆源沉积岩物源分析研究进展与发展趋势, refAbstract=null), Reference(id=1309816826062799330, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2013, volume=31, issue=1, pageStart=99, pageEnd=107, url=null, language=null, rfNumber=[30], rfOrder=59, authorNames=Yang R C, Li J B, Fan A P, Zong M, Zhang T, journalName=Acta Sedimentologica Sinica, refType=null, unstructuredReference=[
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2013. Research progress and development tendency of provenance analysis on terrigenous sedimentary rocks.
Acta Sedimentologica Sinica,
31(1): 99-107], articleTitle=Research progress and development tendency of provenance analysis on terrigenous sedimentary rocks, refAbstract=null), Reference(id=1309816826339623395, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2003, volume=21, issue=3, pageStart=409, pageEnd=415, url=null, language=null, rfNumber=[31], rfOrder=60, authorNames=赵红格, 刘池洋, journalName=沉积学报, refType=null, unstructuredReference=赵红格, 刘池洋.
2003. 物源分析方法及研究进展.
沉积学报,
21(3): 409-415., articleTitle=物源分析方法及研究进展, refAbstract=null), Reference(id=1309816826427703780, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2003, volume=21, issue=3, pageStart=409, pageEnd=415, url=null, language=null, rfNumber=[31], rfOrder=61, authorNames=Zhao H G, Liu C Y, journalName=Acta Sedimentologica Sinica, refType=null, unstructuredReference=[
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2003. Approaches and prospects of provenance analysis.
Acta Sedimentologica Sinica,
21(3): 409-415], articleTitle=Approaches and prospects of provenance analysis, refAbstract=null), Reference(id=1309816826494812645, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2014, volume=32, issue=1, pageStart=68, pageEnd=77, url=null, language=null, rfNumber=[32], rfOrder=62, authorNames=赵雪松, 高志勇, 冯佳睿, 李小陪, 郭美丽, journalName=沉积学报, refType=null, unstructuredReference=赵雪松, 高志勇, 冯佳睿, 李小陪, 郭美丽.
2014. 库车前陆盆地三叠系—新近系重矿物组合特征与盆山构造演化关系.
沉积学报,
32(1): 68-77., articleTitle=库车前陆盆地三叠系—新近系重矿物组合特征与盆山构造演化关系, refAbstract=null), Reference(id=1309816826599670246, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2014, volume=32, issue=1, pageStart=68, pageEnd=77, url=null, language=null, rfNumber=[32], rfOrder=63, authorNames=Zhao X S, Gao Z Y, Feng J R, Li X P, Guo M L, journalName=Acta Sedimentology Sinica, refType=null, unstructuredReference=[
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2014. Triassic-Neogene heavy minerals'assemblages characteristics and basin-orogen tectonic evolution relationship in the Kuqa foreland basin.
Acta Sedimentology Sinica,
32(1): 68-77], articleTitle=Triassic-Neogene heavy minerals'assemblages characteristics and basin-orogen tectonic evolution relationship in the Kuqa foreland basin, refAbstract=null), Reference(id=1309816826738082280, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2025, volume=46, issue=2, pageStart=599, pageEnd=616, url=null, language=null, rfNumber=[33], rfOrder=64, authorNames=张倩, journalName=石油与天然气地质, refType=null, unstructuredReference=张倩.
2025. 多方法约束的复杂物源示踪: 以渤海湾盆地东营凹陷古近系孔店组—沙河街组四段下亚段为例.
石油与天然气地质,
46(2): 599-616., articleTitle=多方法约束的复杂物源示踪: 以渤海湾盆地东营凹陷古近系孔店组—沙河街组四段下亚段为例, refAbstract=null), Reference(id=1309816826821968361, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2025, volume=46, issue=2, pageStart=599, pageEnd=616, url=null, language=null, rfNumber=[33], rfOrder=65, authorNames=Zhang Q, journalName=Oil & Gas Geology, refType=null, unstructuredReference=[
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2025. Multi-method-constrained tracing of complex provenance: a case study of the sequence from the Paleogene Kongdian Formation to the lower submember of the 4th member of the Shahejie Formation in the dongying sag.
Oil & Gas Geology,
46(2): 599-616], articleTitle=Multi-method-constrained tracing of complex provenance: a case study of the sequence from the Paleogene Kongdian Formation to the lower submember of the 4th member of the Shahejie Formation in the dongying sag, refAbstract=null), Reference(id=1309816826910048746, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2025, volume=27, issue=4, pageStart=886, pageEnd=902, url=null, language=null, rfNumber=[34], rfOrder=66, authorNames=张釜源, 祝海华, 张本健, 王明磊, 林思臣, 张芮, 杨希琳, 李育聪, 王兴志, journalName=古地理学报, refType=null, unstructuredReference=张釜源, 祝海华, 张本健, 王明磊, 林思臣, 张芮, 杨希琳, 李育聪, 王兴志.
2025. 四川盆地中侏罗统凉高山组物源特征及沉积演化模式.
古地理学报,
27(4): 886-902., articleTitle=四川盆地中侏罗统凉高山组物源特征及沉积演化模式, refAbstract=null), Reference(id=1309816826985546219, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2025, volume=27, issue=4, pageStart=886, pageEnd=902, url=null, language=null, rfNumber=[34], rfOrder=67, authorNames=Zhang F Y, Zhu H H, Zhang B J, Wang M L, Lin S C, Zhang R, Yang X L, Li Y C, Wang X Z, journalName=Journal of Palaeogeography(Chinese Edition), refType=null, unstructuredReference=[
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2025. Provenance characteristics and sedimentary evolutionary model of the Middle Jurassic Lianggaoshan Formation,Sichuan Basin.
Journal of Palaeogeography(Chinese Edition),
27(4): 886-902], articleTitle=Provenance characteristics and sedimentary evolutionary model of the Middle Jurassic Lianggaoshan Formation,Sichuan Basin, refAbstract=null), Reference(id=1309816827061043692, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=2015, volume=26, issue=4, pageStart=667, pageEnd=678, url=null, language=null, rfNumber=[35], rfOrder=68, authorNames=张荣虎, 王俊鹏, 马玉杰, 陈戈, 曾庆鲁, 周晨光, journalName=天然气地球科学, refType=null, unstructuredReference=张荣虎, 王俊鹏, 马玉杰, 陈戈, 曾庆鲁, 周晨光.
2015. 塔里木盆地库车坳陷深层沉积微相古地貌及其对天然气富集的控制.
天然气地球科学,
26(4): 667-678., articleTitle=塔里木盆地库车坳陷深层沉积微相古地貌及其对天然气富集的控制, refAbstract=null), Reference(id=1309816827123958253, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, doi=null, pmid=null, pmcid=null, year=null, volume=26, issue=4, pageStart=667, pageEnd=678, url=null, language=null, rfNumber=[35], rfOrder=69, authorNames=Zhang R H, Wang J P, Ma Y J, Chen G, Zeng Q L, Zhou C G, journalName=Natural Gas Geoscience, refType=null, unstructuredReference=[
Zhang R H,
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Zhou C G.2015. The sedimentary microfacies, palaeogeomorphology and their controls on gas accumulation of deep-buried Cretaceous in Kuqa Depression,Tarim Basin,China.
Natural Gas Geoscience,
26(4): 667-678], articleTitle=palaeogeomorphology and their controls on gas accumulation of deep-buried Cretaceous in Kuqa Depression,Tarim Basin,China, refAbstract=null)], funds=[Fund(id=1309816818827624866, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, awardId=2024DJ8606, language=EN, fundingSource=Science and Technology Project Topic of PetroChina(2024DJ8606), fundOrder=null, country=null), Fund(id=1309816818907316643, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, awardId=2024DJ8606, language=CN, fundingSource=*中国石油天然气股份有限公司科技项目课题(2024DJ8606), fundOrder=null, country=null)], companyList=[AuthorCompany(id=1309816809273000264, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, xref=1, ext=[AuthorCompanyExt(id=1309816809285583177, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, companyId=1309816809273000264, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=
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2 Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, China), AuthorCompanyExt(id=1309816809566601549, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, companyId=1309816809541435723, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=
2 中国石油勘探开发研究院, 北京 100083)])], figs=[ArticleFig(id=1309816814226473350, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=EN, label=Fig.1, caption=
Plan view of Kelasu structural belt in Kuqa Depression and key gas reservoirs in the Kela-Keshen gas field, figureFileSmall=sRR6fPL66h8rdzjoSFXjag==, figureFileBig=yjA6T7YUdcB9x83fkrWkjg==, tableContent=null), ArticleFig(id=1309816814318748040, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=CN, label=图1, caption=
库车坳陷克拉苏构造带与克拉—克深气田重点气藏分布平面图 a-塔里木盆地库车坳陷位置平面图; b-克拉苏构造带位置平面图; c-研究区克拉—克深气田重点钻井分布图;d-库车坳陷白垩系巴什基奇克组沉积相平面图
, figureFileSmall=sRR6fPL66h8rdzjoSFXjag==, figureFileBig=yjA6T7YUdcB9x83fkrWkjg==, tableContent=null), ArticleFig(id=1309816814822064521, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=EN, label=Fig.2, caption=
Heavy mineral assemblages and ZTR index distribution characteristics of the Kela 2-Keshen 2-Keshen 8-Keshen 9-Keshen 13 gas reservoir in eastern Keshen area, figureFileSmall=ATn4GoCrrkRFdqQXkbKUSw==, figureFileBig=RB4QGgHpErHuI2QnYELaJQ==, tableContent=null), ArticleFig(id=1309816814998225290, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=CN, label=图2, caption=
克深地区东部克拉2-克深2-克深8-克深9-克深13气藏砂岩重矿物组合与ZTR指数分布特征平面图, figureFileSmall=ATn4GoCrrkRFdqQXkbKUSw==, figureFileBig=RB4QGgHpErHuI2QnYELaJQ==, tableContent=null), ArticleFig(id=1309816815073722763, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=EN, label=Fig.3, caption=
Heavy mineral assemblages and ZTR index distribution characteristics of the Keshen 11-Keshen 5-Keshen 24-Keshen 31 gas reservoir in western Keshen area, figureFileSmall=HSkT0WieGaWPsk8Ivlt5Bg==, figureFileBig=FDa9YXJDJEaVRqRIudOhGQ==, tableContent=null), ArticleFig(id=1309816815145025932, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=CN, label=图3, caption=
克深地区西部克深11-克深5-克深24-克深31气藏砂岩重矿物组合与ZTR指数分布特征平面图, figureFileSmall=HSkT0WieGaWPsk8Ivlt5Bg==, figureFileBig=FDa9YXJDJEaVRqRIudOhGQ==, tableContent=null), ArticleFig(id=1309816815430238605, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=EN, label=Fig.4, caption=
Zonation of heavy mineral assemblage characteristics of the Bashijiqike Formation sandstones in Keshen area and distribution of indicated provenance transport channels, figureFileSmall=l0JZS6xpqjYEkswAWNahgg==, figureFileBig=I/qq+dhhnxmXF9qrPh9TUg==, tableContent=null), ArticleFig(id=1309816815493153166, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=CN, label=图4, caption=
克深地区巴什基奇克组砂岩重矿物组合特征分类及指示的物源通道分布, figureFileSmall=l0JZS6xpqjYEkswAWNahgg==, figureFileBig=I/qq+dhhnxmXF9qrPh9TUg==, tableContent=null), ArticleFig(id=1309816815581233551, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=EN, label=Fig.5, caption=
Microstructural characteristics of K-feldspar and plagioclase in sandstones of the Keshen area under microscope and cathodoluminescence, figureFileSmall=pfGkf5m0UOnOYDX9E6DCiA==, figureFileBig=Gr75A6cOIVxtUElTASHgWQ==, tableContent=null), ArticleFig(id=1309816815686091152, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=CN, label=图5, caption=
克深地区砂岩中钾长石、斜长石显微镜与阴极发光下微观结构特征 a—克深301井,井深6842.16 m,中粒岩屑长石砂岩,钾长石(Pf)与斜长石(Pl)及石英(Q);b—与a同一视域阴极发光,钾长石(Pf)发亮蓝色光,斜长石(Pl)发棕色光,石英(Q)发棕色光; c—克深601井,井深6095.78 m,中粒岩屑长石砂岩,钾长石(Pf)及石英(Q);d—与c同一视域阴极发光,钾长石(Pf)发亮蓝色光,石英(Q)发棕色光; e—克深904井,井深7850.8 m,中粒岩屑长石砂岩,钾长石(Pf)与斜长石(Pl)及石英(Q);f—与e同一视域阴极发光,钾长石(Pf)发亮蓝色光,斜长石(Pl)发棕色光、淡绿色光,石英(Q)发棕色光; g—克深4井,井深3393.3 m,中粗粒长石岩屑砂岩,钾长石(Pf)、石英(Q)及花岗岩岩屑(GC);h—与g同一视域阴极发光,钾长石(Pf)发亮蓝色光,石英(Q)发棕色光,花岗岩岩屑(GC)是二者结合体
, figureFileSmall=pfGkf5m0UOnOYDX9E6DCiA==, figureFileBig=Gr75A6cOIVxtUElTASHgWQ==, tableContent=null), ArticleFig(id=1309816815837086097, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=EN, label=Fig.6, caption=
Comparison of variations in detrital component contents of the Bashijiqike Formation sandstones in different wells in Keshen area, figureFileSmall=7ncStA7d0XfUKOa4IYj7Bw==, figureFileBig=Yj6/peJ6L9sh5uWRlyoxYQ==, tableContent=null), ArticleFig(id=1309816815908389266, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=CN, label=图6, caption=
克深地区巴什基奇克组各井砂岩碎屑组分含量变化特征对比, figureFileSmall=7ncStA7d0XfUKOa4IYj7Bw==, figureFileBig=Yj6/peJ6L9sh5uWRlyoxYQ==, tableContent=null), ArticleFig(id=1309816815983886739, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=EN, label=Fig.7, caption=
Average content of various clastic components in Bashijiqike Formation in Keshen area, figureFileSmall=ThKUDWTm2EEjc/7g4Im0Sg==, figureFileBig=PGm0JtrnUy7Tt77WE1XSng==, tableContent=null), ArticleFig(id=1309816816059384212, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=CN, label=图7, caption=
克深地区巴什基奇克组各碎屑组分平均含量平面分布 a—钾长石平均含量等值线图;b—斜长石平均含量等值线图;c—变质岩岩屑平均含量等值线图
, figureFileSmall=ThKUDWTm2EEjc/7g4Im0Sg==, figureFileBig=PGm0JtrnUy7Tt77WE1XSng==, tableContent=null), ArticleFig(id=1309816816273293717, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=EN, label=Fig.8, caption=
Division of provenance transport channels in the Bashijiqike Formation in Keshen area, figureFileSmall=4L/wlyhxblF8yvO6+va7Uw==, figureFileBig=3TDy7fCWX6RSLeqfS0Zq4Q==, tableContent=null), ArticleFig(id=1309816816357179798, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=CN, label=图8, caption=
克深地区巴什基奇克组物源输送通道精细分区平面分布, figureFileSmall=4L/wlyhxblF8yvO6+va7Uw==, figureFileBig=3TDy7fCWX6RSLeqfS0Zq4Q==, tableContent=null), ArticleFig(id=1309816816684335511, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=EN, label=Fig.9, caption=
Sedimentary model of fluvial-dominated braided delta in the Bashijiqike Formation in Keshen area, figureFileSmall=Io4mzcZpXfueEzt7rsyFkA==, figureFileBig=JbcQpI2Hvx+PLmeglpkfFg==, tableContent=null), ArticleFig(id=1309816816780804504, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=CN, label=图9, caption=
克深地区巴什基奇克组河控辫状河三角洲沉积模式, figureFileSmall=Io4mzcZpXfueEzt7rsyFkA==, figureFileBig=JbcQpI2Hvx+PLmeglpkfFg==, tableContent=null), ArticleFig(id=1309816817095377305, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=EN, label=Table 1, caption=
Heavy mineral content of the Bashijiqike Formation sandstones in wells Kela 203 and Keshen 902
, figureFileSmall=null, figureFileBig=null, tableContent=
| 井名 | 层位 | 井深 /m | 重矿物类型及含量/% | 重矿物组合 |
| 锆石 | 电气石 | 金红石 | 石榴子石 | 磷灰石 | 磁铁矿 | 云母 | 绿泥石 | 绿帘石 | 榍石 | 白钛石 |
克拉 203井 | 巴二段 | 3837.49 | 3.30 | 4.60 | / | 4.30 | 9.30 | 56.90 | / | 0.60 | / | 1.70 | / | 锆石+电气石+金红石+石榴子石+磷灰石+磁铁矿+云母+绿泥石+榍石+绿帘石 |
| 3835.22 | 2.70 | 5.60 | / | 5.60 | 5.60 | 52.80 | / | 8.30 | 8.30 | 2.70 | / |
| 3840.79 | 3.10 | 2.50 | 0.60 | 1.20 | 16.00 | 36.40 | / | 3.10 | / | 3.70 | / |
| 3844.71 | 4.90 | 3.50 | / | 3.80 | 7.00 | 51.20 | 0.70 | 0.30 | 0.30 | 2.10 | / |
| 3848.12 | 4.20 | 2.10 | 0.20 | 0.80 | 8.90 | 59.60 | 1.90 | 1.50 | / | 0.80 | / |
| 3850.58 | 6.90 | 1.60 | / | 0.60 | 17.00 | 54.70 | 1.20 | 2.10 | / | 1.80 | / |
| 3853.62 | 10.70 | 2.90 | 0.10 | 0.40 | 9.60 | 57.60 | 0.50 | 0.70 | / | 1.00 | / |
| 3855.55 | 6.00 | 2.50 | 0.20 | / | 1.00 | 49.10 | / | 1.20 | / | 1.70 | / |
| 3856.55 | 3.10 | 2.10 | / | 0.50 | 3.90 | 25.60 | 1.30 | 3.70 | / | 0.30 | / |
| 3858.65 | 2.90 | 40.00 | / | / | 3.40 | 19.00 | 0.60 | | / | 1.10 | / |
| 巴三段 | 4014.20 | 1.30 | 1.50 | 0.10 | 8.70 | 4.40 | 34.20 | / | 10.10 | / | 0.80 | / |
| 4014.88 | 0.90 | 0.90 | / | 2.40 | 8.30 | 10.10 | / | 42.70 | / | 0.50 | / |
| 4016.21 | 0.90 | 1.00 | 0.10 | 8.90 | 5.50 | 24.00 | 0.30 | 12.20 | / | 0.80 | / |
克深 902井 | 巴二段 | 7926.72 | 7.17 | 2.71 | / | 0.19 | / | 68.22 | / | / | / | / | 9.30 | 锆石+电气石+石榴子石+磁铁矿+白钛石,无金红石、磷灰石、云母、绿帘石,个别绿泥石、榍石等 |
| 7927.41 | 2.13 | 2.89 | / | 0.61 | / | 23.71 | / | / | / | / | 9.88 |
| 7929.31 | 6.33 | 3.09 | / | / | / | 61.56 | / | / | / | / | 12.37 |
| 7930.09 | 3.55 | 1.87 | / | / | / | 50.28 | / | / | / | / | 8.22 |
| 7931.35 | 1.14 | 2.51 | / | 0.23 | / | 43.96 | / | / | / | / | 25.28 |
| 7932.02 | 3.11 | 5.26 | / | / | / | 65.55 | / | / | / | / | 13.16 |
| 巴二段 | 7972.43 | 2.92 | 2.77 | / | 0.58 | / | 38.25 | / | / | / | / | 11.39 |
| 7973.27 | 3.58 | 2.83 | / | 0.30 | / | 46.20 | / | / | / | 0.15 | 8.49 |
| 7973.98 | 1.60 | 1.60 | / | 0.96 | / | 32.37 | / | / | / | / | 5.45 |
| 7975.84 | 2.89 | 1.93 | / | 0.24 | / | 30.12 | / | 0.24 | / | / | 3.61 |
), ArticleFig(id=1309816817212817818, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=CN, label=表1, caption=
克拉203井与克深902井巴什基奇克组砂岩重矿物数据
, figureFileSmall=null, figureFileBig=null, tableContent=
| 井名 | 层位 | 井深 /m | 重矿物类型及含量/% | 重矿物组合 |
| 锆石 | 电气石 | 金红石 | 石榴子石 | 磷灰石 | 磁铁矿 | 云母 | 绿泥石 | 绿帘石 | 榍石 | 白钛石 |
克拉 203井 | 巴二段 | 3837.49 | 3.30 | 4.60 | / | 4.30 | 9.30 | 56.90 | / | 0.60 | / | 1.70 | / | 锆石+电气石+金红石+石榴子石+磷灰石+磁铁矿+云母+绿泥石+榍石+绿帘石 |
| 3835.22 | 2.70 | 5.60 | / | 5.60 | 5.60 | 52.80 | / | 8.30 | 8.30 | 2.70 | / |
| 3840.79 | 3.10 | 2.50 | 0.60 | 1.20 | 16.00 | 36.40 | / | 3.10 | / | 3.70 | / |
| 3844.71 | 4.90 | 3.50 | / | 3.80 | 7.00 | 51.20 | 0.70 | 0.30 | 0.30 | 2.10 | / |
| 3848.12 | 4.20 | 2.10 | 0.20 | 0.80 | 8.90 | 59.60 | 1.90 | 1.50 | / | 0.80 | / |
| 3850.58 | 6.90 | 1.60 | / | 0.60 | 17.00 | 54.70 | 1.20 | 2.10 | / | 1.80 | / |
| 3853.62 | 10.70 | 2.90 | 0.10 | 0.40 | 9.60 | 57.60 | 0.50 | 0.70 | / | 1.00 | / |
| 3855.55 | 6.00 | 2.50 | 0.20 | / | 1.00 | 49.10 | / | 1.20 | / | 1.70 | / |
| 3856.55 | 3.10 | 2.10 | / | 0.50 | 3.90 | 25.60 | 1.30 | 3.70 | / | 0.30 | / |
| 3858.65 | 2.90 | 40.00 | / | / | 3.40 | 19.00 | 0.60 | | / | 1.10 | / |
| 巴三段 | 4014.20 | 1.30 | 1.50 | 0.10 | 8.70 | 4.40 | 34.20 | / | 10.10 | / | 0.80 | / |
| 4014.88 | 0.90 | 0.90 | / | 2.40 | 8.30 | 10.10 | / | 42.70 | / | 0.50 | / |
| 4016.21 | 0.90 | 1.00 | 0.10 | 8.90 | 5.50 | 24.00 | 0.30 | 12.20 | / | 0.80 | / |
克深 902井 | 巴二段 | 7926.72 | 7.17 | 2.71 | / | 0.19 | / | 68.22 | / | / | / | / | 9.30 | 锆石+电气石+石榴子石+磁铁矿+白钛石,无金红石、磷灰石、云母、绿帘石,个别绿泥石、榍石等 |
| 7927.41 | 2.13 | 2.89 | / | 0.61 | / | 23.71 | / | / | / | / | 9.88 |
| 7929.31 | 6.33 | 3.09 | / | / | / | 61.56 | / | / | / | / | 12.37 |
| 7930.09 | 3.55 | 1.87 | / | / | / | 50.28 | / | / | / | / | 8.22 |
| 7931.35 | 1.14 | 2.51 | / | 0.23 | / | 43.96 | / | / | / | / | 25.28 |
| 7932.02 | 3.11 | 5.26 | / | / | / | 65.55 | / | / | / | / | 13.16 |
| 巴二段 | 7972.43 | 2.92 | 2.77 | / | 0.58 | / | 38.25 | / | / | / | / | 11.39 |
| 7973.27 | 3.58 | 2.83 | / | 0.30 | / | 46.20 | / | / | / | 0.15 | 8.49 |
| 7973.98 | 1.60 | 1.60 | / | 0.96 | / | 32.37 | / | / | / | / | 5.45 |
| 7975.84 | 2.89 | 1.93 | / | 0.24 | / | 30.12 | / | 0.24 | / | / | 3.61 |
), ArticleFig(id=1309816817514807707, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=EN, label=Table 2, caption=
Average heavy mineral content and ZTR index of sandstones from the Bashijiqike Formation in Kela 2-Keshen2-Keshen 8-Keshen 9-Keshen 13 gas reservoirs in eastern Keshen area
, figureFileSmall=null, figureFileBig=null, tableContent=
| 井名/样品数 | 主要重矿物平均含量/%(赤褐铁矿平均含量为11.8%~53.69%,不计入) | ZTR指数 |
| 锆石 | 电气石 | 金红石 | 石榴子石 | 磷灰石 | 磁铁矿 | 云母 | 绿泥石 | 绿帘石 | 榍石 | 辉石 | 十字石 | 白钛石 |
| 克拉2井/46 | 3.9 | 0.7 | 0.4 | 0.4 | 3.9 | 25.1 | 0.6 | 1.7 | 0.7 | / | / | / | / | 5.0 |
| 克拉201井/24 | 4.6 | 1.8 | 0.6 | 2.6 | 7.8 | 30.6 | 0.9 | 2.9 | / | 1.4 | / | / | 0.5 | 7.0 |
| 克拉203井/12 | 3.9 | 2.7 | 0.2 | 3.4 | 7.7 | 40.9 | 0.9 | 7.2 | 4.3 | 1.5 | / | / | / | 6.8 |
| 克拉204井/4 | 1.8 | 1.7 | 0.6 | 7.2 | 7.5 | 30.0 | / | 5.2 | / | 2.0 | / | / | / | 4.1 |
| 克深201井/8 | 4.3 | 1.6 | / | 0.4 | / | 42.6 | / | / | / | / | 0.3 | / | 7.6 | 5.9 |
| 克深202井/11 | 8.9 | 3.7 | / | 5.3 | 2.0 | 55.1 | 0.2 | 5.2 | / | / | / | / | 5.0 | 12.6 |
| 克深205井/16 | 2.6 | 3.0 | / | 0.4 | 0.2 | 44.3 | 0.5 | 1.5 | 0.3 | 0.3 | 0.2 | 0.2 | 12.7 | 5.6 |
| 克深206井/10 | 2.3 | 2.4 | 0.3 | 0.2 | / | 25.1 | 0.9 | 0.7 | / | / | / | / | 10.7 | 5.0 |
| 克深207井/49 | 3.4 | 2.6 | 0.3 | 0.3 | 0.4 | 52.0 | 0.3 | 0.4 | 0.2 | 0.2 | / | / | 13.2 | 6.3 |
| 克深1003井/23 | 6.4 | 2.0 | / | 2.6 | 1.0 | 46.0 | 2.0 | 1.5 | / | 0.5 | / | / | 9.0 | 8.4 |
| 克深8井/24 | 3.7 | 2.3 | 0.2 | 0.2 | 0.6 | 39.3 | 0.4 | 0.5 | 0.3 | 0.2 | / | / | 9.9 | 6.2 |
| 克深801井/12 | 1.4 | 1.8 | / | 0.9 | / | 48.7 | / | 0.5 | 0.4 | 0.3 | / | / | 9.9 | 3.2~6.4 |
| 克深802井/10 | 1.6 | 2.8 | / | 0.3 | / | 49.7 | 31.1 | 0.3 | / | 0.3 | / | / | 14.2 | 4.4 |
| 克深8004井/9 | 2.5 | 2.0 | / | 0.8 | / | 41.5 | 0.5 | 0.3 | / | 0.3 | / | / | 7.9 | 4.5 |
| 克深902井/11 | 3.5 | 2.7 | / | 0.4 | / | 48.3 | / | 0.2 | / | 0.2 | / | / | 10.7 | 6.2 |
| 克深904井/27 | 2.4 | 2.1 | 0.2 | 0.5 | / | 52.2 | / | 0.3 | / | 0.2 | / | / | 13.4 | 4.5 |
| 克深12井/9 | 4.2 | 3.0 | / | 0.7 | / | 56.0 | / | / | 0.2 | / | / | / | 17.6 | 7.2 |
| 克深13井/10 | 1.9 | 2.3 | / | 0.2 | / | 39.5 | / | 0.2 | / | 0.1 | / | / | 14.4 | 4.2~7.8 |
| 克深131井/3 | 6.0 | 1.9 | / | 0.5 | / | 58.9 | / | / | 0.2 | / | / | / | 7.3 | 7.9 |
| 克深134井/24 | 4.8 | 1.5 | / | 0.5 | 1.6 | 69.7 | 0.4 | 0.6 | / | / | / | / | 5.7 | 6.3~10.2 |
), ArticleFig(id=1309816817653219740, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=CN, label=表2, caption=
克深地区东部克拉2-克深2-克深8-克深9-克深13气藏巴什基奇克组砂岩重矿物平均含量与ZTR指数数据
, figureFileSmall=null, figureFileBig=null, tableContent=
| 井名/样品数 | 主要重矿物平均含量/%(赤褐铁矿平均含量为11.8%~53.69%,不计入) | ZTR指数 |
| 锆石 | 电气石 | 金红石 | 石榴子石 | 磷灰石 | 磁铁矿 | 云母 | 绿泥石 | 绿帘石 | 榍石 | 辉石 | 十字石 | 白钛石 |
| 克拉2井/46 | 3.9 | 0.7 | 0.4 | 0.4 | 3.9 | 25.1 | 0.6 | 1.7 | 0.7 | / | / | / | / | 5.0 |
| 克拉201井/24 | 4.6 | 1.8 | 0.6 | 2.6 | 7.8 | 30.6 | 0.9 | 2.9 | / | 1.4 | / | / | 0.5 | 7.0 |
| 克拉203井/12 | 3.9 | 2.7 | 0.2 | 3.4 | 7.7 | 40.9 | 0.9 | 7.2 | 4.3 | 1.5 | / | / | / | 6.8 |
| 克拉204井/4 | 1.8 | 1.7 | 0.6 | 7.2 | 7.5 | 30.0 | / | 5.2 | / | 2.0 | / | / | / | 4.1 |
| 克深201井/8 | 4.3 | 1.6 | / | 0.4 | / | 42.6 | / | / | / | / | 0.3 | / | 7.6 | 5.9 |
| 克深202井/11 | 8.9 | 3.7 | / | 5.3 | 2.0 | 55.1 | 0.2 | 5.2 | / | / | / | / | 5.0 | 12.6 |
| 克深205井/16 | 2.6 | 3.0 | / | 0.4 | 0.2 | 44.3 | 0.5 | 1.5 | 0.3 | 0.3 | 0.2 | 0.2 | 12.7 | 5.6 |
| 克深206井/10 | 2.3 | 2.4 | 0.3 | 0.2 | / | 25.1 | 0.9 | 0.7 | / | / | / | / | 10.7 | 5.0 |
| 克深207井/49 | 3.4 | 2.6 | 0.3 | 0.3 | 0.4 | 52.0 | 0.3 | 0.4 | 0.2 | 0.2 | / | / | 13.2 | 6.3 |
| 克深1003井/23 | 6.4 | 2.0 | / | 2.6 | 1.0 | 46.0 | 2.0 | 1.5 | / | 0.5 | / | / | 9.0 | 8.4 |
| 克深8井/24 | 3.7 | 2.3 | 0.2 | 0.2 | 0.6 | 39.3 | 0.4 | 0.5 | 0.3 | 0.2 | / | / | 9.9 | 6.2 |
| 克深801井/12 | 1.4 | 1.8 | / | 0.9 | / | 48.7 | / | 0.5 | 0.4 | 0.3 | / | / | 9.9 | 3.2~6.4 |
| 克深802井/10 | 1.6 | 2.8 | / | 0.3 | / | 49.7 | 31.1 | 0.3 | / | 0.3 | / | / | 14.2 | 4.4 |
| 克深8004井/9 | 2.5 | 2.0 | / | 0.8 | / | 41.5 | 0.5 | 0.3 | / | 0.3 | / | / | 7.9 | 4.5 |
| 克深902井/11 | 3.5 | 2.7 | / | 0.4 | / | 48.3 | / | 0.2 | / | 0.2 | / | / | 10.7 | 6.2 |
| 克深904井/27 | 2.4 | 2.1 | 0.2 | 0.5 | / | 52.2 | / | 0.3 | / | 0.2 | / | / | 13.4 | 4.5 |
| 克深12井/9 | 4.2 | 3.0 | / | 0.7 | / | 56.0 | / | / | 0.2 | / | / | / | 17.6 | 7.2 |
| 克深13井/10 | 1.9 | 2.3 | / | 0.2 | / | 39.5 | / | 0.2 | / | 0.1 | / | / | 14.4 | 4.2~7.8 |
| 克深131井/3 | 6.0 | 1.9 | / | 0.5 | / | 58.9 | / | / | 0.2 | / | / | / | 7.3 | 7.9 |
| 克深134井/24 | 4.8 | 1.5 | / | 0.5 | 1.6 | 69.7 | 0.4 | 0.6 | / | / | / | / | 5.7 | 6.3~10.2 |
), ArticleFig(id=1309816817930043805, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=EN, label=Table 3, caption=
Average heavy mineral content and ZTR index of sandstones from Bashijiqike Formation in Keshen 11-Keshen 5-Keshen 24-Keshen 31 gas reservoirs in western Keshen area
, figureFileSmall=null, figureFileBig=null, tableContent=
| 井名/样品数 | 主要重矿物平均含量/%(赤褐铁矿平均含量为8.5%~33.6%,不计入) | ZTR指数 |
| 锆石 | 电气石 | 金红石 | 石榴子石 | 磷灰石 | 磁铁矿 | 云母 | 绿泥石 | 绿帘石 | 榍石 | 锡石 | 十字石 | 白钛石 |
| 克深1101井/6 | 4.3 | 0.9 | / | 0.9 | 2.6 | 54.2 | 0.4 | 0.4 | / | / | / | / | 3.6 | 5.2 |
| 克深1102井/7 | 2.6 | 1.7 | / | 8.5 | 3.5 | 42.1 | / | 7.1 | / | / | / | / | 4.0 | 4.3 |
| 克深1103井/19 | 2.7 | 0.5 | / | 1.0 | 1.3 | 41.3 | / | 0.3 | 0.4 | / | / | / | 2.0 | 3.2 |
| 克深501井/39 | 2.4 | 1.8 | 0.2 | 1.0 | / | 41.5 | 0.7 | 0.6 | 0.2 | 0.2 | / | / | 17.6 | 4.4 |
| 克深503井/20 | 2.8 | 1.2 | 0.2 | 0.3 | / | 56.6 | / | 0.2 | 0.6 | 0.1 | / | / | 12.1 | 4.2 |
| 克深504井/27 | 2.0 | 1.5 | 0.2 | 0.7 | / | 36.8 | 0.3 | 0.7 | 0.2 | 0.2 | / | / | 10.8 | 3.7 |
| 克深505井/43 | 2.2 | 1.6 | 0.2 | 1.1 | / | 50.4 | 0.2 | 0.4 | 0.2 | 0.2 | / | / | 15.1 | 4.0 |
| 克深241井/18 | 5.8 | 2.5 | 0.2 | 0.3 | 6.0 | 51.1 | 0.4 | 0.4 | / | / | / | / | 12.1 | 8.5 |
| 克深242井/17 | 4.5 | 2.2 | / | 0.6 | 2.5 | 56.2 | / | 1.1 | / | / | / | / | 6.8 | 6.7 |
| 克深24井/6 | 2.3 | 0.8 | / | / | 6.6 | 62.0 | / | / | / | / | / | / | 2.3 | 3.1 |
| 克深19井/12 | 13.8 | 1.7 | / | / | 1.8 | 61.4 | / | 0.2 | / | / | / | / | 8.3 | 15.5 |
| 克深4井/13 | 2.0 | 1.9 | 0.2 | 10.2 | 0.3 | 51.9 | / | 0.3 | 0.3 | 0.5 | / | / | 5.4 | 4.1 |
| 克深1井/7 | 9.9 | 4.5 | 0.8 | 1.6 | / | 28.9 | / | 1.3 | / | 1.5 | 3.0 | / | 25.0 | 15.2 |
| 克深3101井/15 | 2.1 | 1.4 | / | 2.1 | 1.6 | 46.1 | 0.7 | / | / | / | / | / | 8.0 | 3.5~6.2 |
| 克深3102井/16 | 7.3 | 1.1 | / | 0.2 | 1.7 | 70.2 | / | / | 0.2 | / | / | / | 8.1 | 8.4~14.8 |
), ArticleFig(id=1309816818013929886, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=CN, label=表3, caption=
克深地区西部克深11-克深5-克深24-克深31气藏巴什基奇克组砂岩重矿物平均含量与ZTR指数数据
, figureFileSmall=null, figureFileBig=null, tableContent=
| 井名/样品数 | 主要重矿物平均含量/%(赤褐铁矿平均含量为8.5%~33.6%,不计入) | ZTR指数 |
| 锆石 | 电气石 | 金红石 | 石榴子石 | 磷灰石 | 磁铁矿 | 云母 | 绿泥石 | 绿帘石 | 榍石 | 锡石 | 十字石 | 白钛石 |
| 克深1101井/6 | 4.3 | 0.9 | / | 0.9 | 2.6 | 54.2 | 0.4 | 0.4 | / | / | / | / | 3.6 | 5.2 |
| 克深1102井/7 | 2.6 | 1.7 | / | 8.5 | 3.5 | 42.1 | / | 7.1 | / | / | / | / | 4.0 | 4.3 |
| 克深1103井/19 | 2.7 | 0.5 | / | 1.0 | 1.3 | 41.3 | / | 0.3 | 0.4 | / | / | / | 2.0 | 3.2 |
| 克深501井/39 | 2.4 | 1.8 | 0.2 | 1.0 | / | 41.5 | 0.7 | 0.6 | 0.2 | 0.2 | / | / | 17.6 | 4.4 |
| 克深503井/20 | 2.8 | 1.2 | 0.2 | 0.3 | / | 56.6 | / | 0.2 | 0.6 | 0.1 | / | / | 12.1 | 4.2 |
| 克深504井/27 | 2.0 | 1.5 | 0.2 | 0.7 | / | 36.8 | 0.3 | 0.7 | 0.2 | 0.2 | / | / | 10.8 | 3.7 |
| 克深505井/43 | 2.2 | 1.6 | 0.2 | 1.1 | / | 50.4 | 0.2 | 0.4 | 0.2 | 0.2 | / | / | 15.1 | 4.0 |
| 克深241井/18 | 5.8 | 2.5 | 0.2 | 0.3 | 6.0 | 51.1 | 0.4 | 0.4 | / | / | / | / | 12.1 | 8.5 |
| 克深242井/17 | 4.5 | 2.2 | / | 0.6 | 2.5 | 56.2 | / | 1.1 | / | / | / | / | 6.8 | 6.7 |
| 克深24井/6 | 2.3 | 0.8 | / | / | 6.6 | 62.0 | / | / | / | / | / | / | 2.3 | 3.1 |
| 克深19井/12 | 13.8 | 1.7 | / | / | 1.8 | 61.4 | / | 0.2 | / | / | / | / | 8.3 | 15.5 |
| 克深4井/13 | 2.0 | 1.9 | 0.2 | 10.2 | 0.3 | 51.9 | / | 0.3 | 0.3 | 0.5 | / | / | 5.4 | 4.1 |
| 克深1井/7 | 9.9 | 4.5 | 0.8 | 1.6 | / | 28.9 | / | 1.3 | / | 1.5 | 3.0 | / | 25.0 | 15.2 |
| 克深3101井/15 | 2.1 | 1.4 | / | 2.1 | 1.6 | 46.1 | 0.7 | / | / | / | / | / | 8.0 | 3.5~6.2 |
| 克深3102井/16 | 7.3 | 1.1 | / | 0.2 | 1.7 | 70.2 | / | / | 0.2 | / | / | / | 8.1 | 8.4~14.8 |
), ArticleFig(id=1309816818362057119, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=EN, label=Table 4, caption=
Average content of sandstone detrital components in the Bashijiqike Formation of key wells in Keshen area
, figureFileSmall=null, figureFileBig=null, tableContent=
| 井名/样品数 | 井深/m | 石英/% | 长石/% | 岩屑/% |
| 钾长石 | 斜长石 | 沉积岩 | 变质岩 | 岩浆岩 |
| 克拉201井/35 | 3650.00~3744.00 | 41.2 | 12.9 | 1.3 | 17.4 | 21.5 | 6.5 |
| 克拉2-13井/5 | 4971.10~4986.99 | 50.2 | 14.0 | 5.2 | 4.0 | 18.2 | 8.2 |
| 克深601井/60 | 6080.08~6157.82 | 46.3 | 18.7 | 10.6 | 3.1 | 14.1 | 7.3 |
| 克深602井/65 | 6006.59~6021.12 | 44.9 | 16.4 | 9.3 | 2.6 | 17.3 | 9.4 |
| 6082.27~6096.52 | 50.0 | 15.7 | 9.3 | 2.6 | 13.7 | 8.5 |
| 克深205井/45 | 6931.07~6934.63 | 41.2 | 21.7 | 9.2 | 3.5 | 12.2 | 12.2 |
| 7085.06~7092.98 | 40.8 | 25.8 | 10.4 | 2.3 | 10.8 | 9.9 |
| 7182.00~7219.00 | 42.2 | 20.6 | 8.3 | 2.5 | 8.8 | 17.8 |
| 克深208井/14 | 6597.33~6615.14 | 41.2 | 25.6 | 12.3 | 3.6 | 7.6 | 9.7 |
| 克深301井/15 | 6836.01~6948.43 | 41.3 | 20.3 | 17.6 | 2.3 | 8.5 | 10.0 |
| 克深8井/52 | 6728.07~6740.82 | 41.7 | 22.3 | 9.9 | 2.2 | 13.8 | 10.1 |
| 6825.87~6826.98 | 42.8 | 21.4 | 12.4 | 3.6 | 12.0 | 7.8 |
| 6872.05~6873.64 | 39.0 | 20.5 | 14.3 | 7.0 | 9.8 | 9.5 |
| 克深904井/48 | 7724.44~7740.96 | 44.0 | 18.1 | 15.2 | 2.8 | 9.0 | 10.8 |
| 7849.07~7853.59 | 44.9 | 19.4 | 15.7 | 2.4 | 7.3 | 10.3 |
| 克深134井/5 | 7632.66~7635.07 | 52.0 | 14.2 | 7.4 | 6.4 | 14.0 | 6.0 |
| 克深4井/28 | 3387.29~3395.27 | 36.9 | 26.1 | 1.4 | 5.4 | 14.5 | 16.1 |
| 克深1003井/37 | 6469.75~6572.52 | 44.1 | 20.5 | 7.5 | 3.9 | 16.2 | 7.5 |
| 克深24井/12 | 6178.20~6185.86 | 46.0 | 23.0 | 7.2 | 2.8 | 16.5 | 4.0 |
| 克深242井/18 | 6440.45~6464.94 | 47.4 | 17.1 | 6.4 | 4.1 | 15.7 | 9.1 |
| 6562.17~6568.95 | 45.7 | 13.3 | 15.4 | 3.1 | 13.1 | 9.3 |
| 克深801井/22 | 7201.96~7229.35 | 42.3 | 22.5 | 17.8 | 1.8 | 7.1 | 8.5 |
| 7291.34~7294.18 | 40.6 | 21.0 | 17.6 | 1.6 | 10.4 | 8.8 |
| 7323.4~7327.24 | 42.2 | 22.0 | 17.6 | 2.0 | 9.4 | 6.8 |
| 克深902井/20 | 7816.15~7940.40 | 48.8 | 18.2 | 14.4 | 2.4 | 6.7 | 9.5 |
| 7972.43~7975.84 | 45.8 | 19.0 | 16.5 | 1.7 | 8.5 | 8.2 |
| 克深7井/2 | 7992.00~7994.00 | 40.0 | 30.0 | 10.0 | 3.0 | 5.0 | 12.0 |
| 克深11井/20 | 6266.10~6273.06 | 43.4 | 15.2 | 10.8 | 3.0 | 16.0 | 11.7 |
| 克深1101井/50 | 6596.73~6637.73 | 49.5 | 21.5 | 3.0 | 4.1 | 15.9 | 6.9 |
| 克深5井/7 | 6726.00~6805.00 | 50.7 | 15.2 | 11.0 | 3.3 | 14.3 | 14.7 |
| 克深505井/80 | 6755.11~6793.37 | 47.2 | 16.1 | 11.8 | 4.1 | 11.5 | 9.1 |
| 克深19井/16 | 7873.20~7878.83 | 43.4 | 20.5 | 8.7 | 2.8 | 15.4 | 9.2 |
| 克深21井/20 | 7935.00~8072.00 | 44.9 | 21.0 | 17.9 | 2.2 | 9.9 | 4.7 |
| 克深3101井/40 | 7836.11~7845.30 | 42.3 | 20.0 | 12.1 | 3.2 | 14.8 | 7.5 |
| 克深3103井/7 | 8016.00~8102.00 | 44.7 | 25.7 | 6.0 | 2.7 | 13.9 | 7.1 |
), ArticleFig(id=1309816818492080545, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309816805019975985, language=CN, label=表4, caption=
克深地区重点井巴什基奇克组砂岩碎屑组分平均含量统计
, figureFileSmall=null, figureFileBig=null, tableContent=
| 井名/样品数 | 井深/m | 石英/% | 长石/% | 岩屑/% |
| 钾长石 | 斜长石 | 沉积岩 | 变质岩 | 岩浆岩 |
| 克拉201井/35 | 3650.00~3744.00 | 41.2 | 12.9 | 1.3 | 17.4 | 21.5 | 6.5 |
| 克拉2-13井/5 | 4971.10~4986.99 | 50.2 | 14.0 | 5.2 | 4.0 | 18.2 | 8.2 |
| 克深601井/60 | 6080.08~6157.82 | 46.3 | 18.7 | 10.6 | 3.1 | 14.1 | 7.3 |
| 克深602井/65 | 6006.59~6021.12 | 44.9 | 16.4 | 9.3 | 2.6 | 17.3 | 9.4 |
| 6082.27~6096.52 | 50.0 | 15.7 | 9.3 | 2.6 | 13.7 | 8.5 |
| 克深205井/45 | 6931.07~6934.63 | 41.2 | 21.7 | 9.2 | 3.5 | 12.2 | 12.2 |
| 7085.06~7092.98 | 40.8 | 25.8 | 10.4 | 2.3 | 10.8 | 9.9 |
| 7182.00~7219.00 | 42.2 | 20.6 | 8.3 | 2.5 | 8.8 | 17.8 |
| 克深208井/14 | 6597.33~6615.14 | 41.2 | 25.6 | 12.3 | 3.6 | 7.6 | 9.7 |
| 克深301井/15 | 6836.01~6948.43 | 41.3 | 20.3 | 17.6 | 2.3 | 8.5 | 10.0 |
| 克深8井/52 | 6728.07~6740.82 | 41.7 | 22.3 | 9.9 | 2.2 | 13.8 | 10.1 |
| 6825.87~6826.98 | 42.8 | 21.4 | 12.4 | 3.6 | 12.0 | 7.8 |
| 6872.05~6873.64 | 39.0 | 20.5 | 14.3 | 7.0 | 9.8 | 9.5 |
| 克深904井/48 | 7724.44~7740.96 | 44.0 | 18.1 | 15.2 | 2.8 | 9.0 | 10.8 |
| 7849.07~7853.59 | 44.9 | 19.4 | 15.7 | 2.4 | 7.3 | 10.3 |
| 克深134井/5 | 7632.66~7635.07 | 52.0 | 14.2 | 7.4 | 6.4 | 14.0 | 6.0 |
| 克深4井/28 | 3387.29~3395.27 | 36.9 | 26.1 | 1.4 | 5.4 | 14.5 | 16.1 |
| 克深1003井/37 | 6469.75~6572.52 | 44.1 | 20.5 | 7.5 | 3.9 | 16.2 | 7.5 |
| 克深24井/12 | 6178.20~6185.86 | 46.0 | 23.0 | 7.2 | 2.8 | 16.5 | 4.0 |
| 克深242井/18 | 6440.45~6464.94 | 47.4 | 17.1 | 6.4 | 4.1 | 15.7 | 9.1 |
| 6562.17~6568.95 | 45.7 | 13.3 | 15.4 | 3.1 | 13.1 | 9.3 |
| 克深801井/22 | 7201.96~7229.35 | 42.3 | 22.5 | 17.8 | 1.8 | 7.1 | 8.5 |
| 7291.34~7294.18 | 40.6 | 21.0 | 17.6 | 1.6 | 10.4 | 8.8 |
| 7323.4~7327.24 | 42.2 | 22.0 | 17.6 | 2.0 | 9.4 | 6.8 |
| 克深902井/20 | 7816.15~7940.40 | 48.8 | 18.2 | 14.4 | 2.4 | 6.7 | 9.5 |
| 7972.43~7975.84 | 45.8 | 19.0 | 16.5 | 1.7 | 8.5 | 8.2 |
| 克深7井/2 | 7992.00~7994.00 | 40.0 | 30.0 | 10.0 | 3.0 | 5.0 | 12.0 |
| 克深11井/20 | 6266.10~6273.06 | 43.4 | 15.2 | 10.8 | 3.0 | 16.0 | 11.7 |
| 克深1101井/50 | 6596.73~6637.73 | 49.5 | 21.5 | 3.0 | 4.1 | 15.9 | 6.9 |
| 克深5井/7 | 6726.00~6805.00 | 50.7 | 15.2 | 11.0 | 3.3 | 14.3 | 14.7 |
| 克深505井/80 | 6755.11~6793.37 | 47.2 | 16.1 | 11.8 | 4.1 | 11.5 | 9.1 |
| 克深19井/16 | 7873.20~7878.83 | 43.4 | 20.5 | 8.7 | 2.8 | 15.4 | 9.2 |
| 克深21井/20 | 7935.00~8072.00 | 44.9 | 21.0 | 17.9 | 2.2 | 9.9 | 4.7 |
| 克深3101井/40 | 7836.11~7845.30 | 42.3 | 20.0 | 12.1 | 3.2 | 14.8 | 7.5 |
| 克深3103井/7 | 8016.00~8102.00 | 44.7 | 25.7 | 6.0 | 2.7 | 13.9 | 7.1 |
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