Article(id=1309196910112637518, tenantId=1146029695717560320, journalId=1308397449582313577, issueId=1309196716851687705, articleNumber=null, orderNo=null, doi=10.7605/gdlxb.2026.033, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=research-article, receivedDate=1728144000000, receivedDateStr=2024-10-06, revisedDate=1736179200000, revisedDateStr=2025-01-07, acceptedDate=null, acceptedDateStr=null, onlineDate=1790066467072, onlineDateStr=2026-09-22, pubDate=1769875200000, pubDateStr=2026-02-01, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1790066467072, onlineIssueDateStr=2026-09-22, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1790066467072, creator=13701087609, updateTime=1790066467072, updator=13701087609, issue=Issue{id=1309196716851687705, tenantId=1146029695717560320, journalId=1308397449582313577, year='2026', volume='28', issue='1', pageStart='1', pageEnd='428', issueExtLink='null', onlineDate='null', pubDate='1769875200000', pubDateStr='2026-02-01', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=1, issueType=-1, specialIssue=null, createTime=1790066420995, creator='13701087609', updateTime=1790156970446, updator='13701087609', preIssue=null, nextIssue=null, articleTotal=null, ext={EN=IssueExt(id=1309576508830740850, tenantId=1146029695717560320, journalId=1308397449582313577, issueId=1309196716851687705, language=EN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=), CN=IssueExt(id=1309576508830740851, tenantId=1146029695717560320, journalId=1308397449582313577, issueId=1309196716851687705, language=CN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=)}, issueFiles=null, downloadFileDto=null}, startPage=127, endPage=145, ext={EN=ArticleExt(id=1309196910330741327, articleId=1309196910112637518, tenantId=1146029695717560320, journalId=1308397449582313577, language=EN, title=Sedimentary facies of the Triassic Lower Karamay Formation of Xia 77 area in northwest margin of Junggar Basin, columnId=1309196717719908635, journalTitle=Journal of Palaeogeography (Chinese Edition), columnName=LITHOFACIES PALAEOGEOGRAPHY AND SEDIMENTOLOGY, runingTitle=null, highlight=null, articleAbstract=

The Triassic Lower Karamay Formation(T₂k₁)represents the primary target for petroleum exploration in the Xia 77 area,located on the northwest margin of Junggar Basin. Integrating data from drilling,core observations,well logging,and associated analytical experiments,this study applies fundamental principles of sedimentology to analyze the sedimentary facies architecture and evolutionary characteristics of the T₂k₁. The findings reveal the following: (1)The formation was deposited within a shallow-water fan delta system,which is subdivided into two main subfacies: the fan delta plain and the fan delta front. The fan delta front can be further classified into inner and outer front subfacies.(2)Within the fan delta plain,three gravity flow-dominated microfacies were identified: braided channels,floodplains,and debris flows. In the fan delta inner front,two traction flow-dominated microfacies are recognized—subaqueous distributary channels and subaqueous distributary bays. The fan delta outer front is characterized by three traction flow-induced microfacies: subaqueous distributary channels,subaqueous distributary bays,and mouth bars.(3)During the depositional period of the Lower Karamay Formation,the lake basin underwent a gradual deepening,transitioning from shallow to deeper water conditions. This hydrodynamic shift resulted in a regressive sedimentary sequence in response to overall lake transgression. Laterally,the progradational-to-retrogradational evolution of the system led to a northeastward backstepping of the fan delta plain,inner front,and outer front subfacies.

, authors=Chao DING¹, Chunming LIN², Jun LIU¹, Weihang WEI², Guyue TAN², Xia ZHANG², Shuya HUANG², Xiaolong LIU¹, Zhen CHEN¹, Sutian WANG¹, authorsList=Chao DING, Chunming LIN, Jun LIU, Weihang WEI, Guyue TAN, Xia ZHANG, Shuya HUANG, Xiaolong LIU, Zhen CHEN, Sutian WANG, authorCompany=null, correspAuthors=Chunming LIN, authorNote=, correspAuthorsNote=, copyrightStatement=null, copyrightOwner=null, extLink=null, articleAbsUrl=null, sourceXml=null, magXml=null, pdfUrl=null, pdf=null, pdfFileSize=null, pdfExtLink=null, richHtmlUrl=null, mobilePdfUrl=null, reviewReport=null, pdfFirstPage=null, abstractGraph=null, abstractGraphContent=null, abstractVideo=null, citation=null, cebUrl=null, magXmlContent=null, mapNumber=null, fund=null), CN=ArticleExt(id=1309196914030117480, articleId=1309196910112637518, tenantId=1146029695717560320, journalId=1308397449582313577, language=CN, title=准噶尔盆地西北缘夏77地区三叠系克下组沉积相研究^*, columnId=1309196717900263709, journalTitle=古地理学报, columnName=岩相古地理学及沉积学, runingTitle=null, highlight=null, articleAbstract=

准噶尔盆地西北缘夏77地区三叠系克下组(克拉玛依下亚组,T₂k₁)是油气勘探的重点目的层系。综合钻井、岩心、录测井和分析化验等资料,运用沉积学基本原理和方法,开展了克下组的沉积相及其演化特征研究。 结果表明: (1)夏77地区克下组主要发育浅水扇三角洲沉积,划分为扇三角洲平原和扇三角洲前缘亚相,前缘亚相又分内前缘和外前缘。(2)扇三角洲平原亚相发育重力流成因辫状河道、漫滩和碎屑流3种微相;内前缘识别出水下分流河道和水下分流间湾2种微相,牵引流成因较强、重力流成因较弱;外前缘发育牵引流成因水下分流河道、水下分流间湾和河口坝3种微相。(3)克下组沉积时期,湖盆水体由浅变深,地层表现为湖侵退积沉积序列,平面上,扇三角洲平原、内前缘和外前缘亚相向东北方向后退。

, authors=丁超¹, 林春明², 刘军¹, 魏维航², 谭古月², 张霞², 黄舒雅², 刘晓龙¹, 陈朕¹, 王苏天¹, authorsList=丁超, 林春明, 刘军, 魏维航, 谭古月, 张霞, 黄舒雅, 刘晓龙, 陈朕, 王苏天, authorCompany=null, correspAuthors=林春明, authorNote=, correspAuthorsNote=, copyrightStatement=null, copyrightOwner=null, extLink=null, articleAbsUrl=null, sourceXml=joH7rlu7q4KSH5WkCtV+hQ==, magXml=BU/IcR9JNvBbYj/IfN9Csg==, pdfUrl=null, pdf=8alsR9wEsE8zImf6xKhn3Q==, pdfFileSize=16463635, pdfExtLink=null, richHtmlUrl=null, mobilePdfUrl=null, reviewReport=null, pdfFirstPage=null, abstractGraph=FHoRaukDuUfgnx8yvzLiWQ==, abstractGraphContent=null, abstractVideo=null, citation=null, cebUrl=null, magXmlContent=rJyV+mAoVmxk6kMal9hyZg==, mapNumber=null, fund=null)}, authors=[Author(id=1309196914562794096, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, orderNo=0, firstName=null, middleName=null, lastName=null, nameCn=null, orcid=null, stid=null, country=null, authorPic=null, dead=0, email=ptrdc@petroChina.com.cn, emailSecond=null, emailThird=null, correspondingAuthor=0, authorType=1, ext={EN=AuthorExt(id=1309196914625708658, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, authorId=1309196914562794096, language=EN, stringName=Chao DING, firstName=Chao, middleName=null, lastName=DING, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=¹, address=1 PetroChina Xinjiang Oilfield Company,Xinjiang Karamay 834000,China, bio={"content":"

DING Chao,born in 1982,is a senior engineer. He is mainly engaged in the comprehensive research and management of petroleum geology. E-mail: ptrdc@petroChina.com.cn.

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DING Chao,born in 1982,is a senior engineer. He is mainly engaged in the comprehensive research and management of petroleum geology. E-mail: ptrdc@petroChina.com.cn.

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丁超,男,1982年生,高级工程师,主要从事石油地质综合研究及管理工作。E-mail: ptrdc@petroChina.com.cn。

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丁超,男,1982年生,高级工程师,主要从事石油地质综合研究及管理工作。E-mail: ptrdc@petroChina.com.cn。

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Petroleum Science, 13(3): 385-401., articleTitle=Sedimentary characteristics and processes of Paleogene Dainan Formation in the Gaoyou Depression,North Jiangsu Basin,Eastern China, refAbstract=null), Reference(id=1309196932619272987, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, doi=null, pmid=null, pmcid=null, year=2018, volume=130, issue=3-4, pageStart=455, pageEnd=483, url=null, language=null, rfNumber=[45], rfOrder=76, authorNames=Zhang X, Dalrymple W, Lin C M, journalName=Geological Society of America Bulletin, refType=null, unstructuredReference=Zhang X, Dalrymple W, Lin C M. 2018. Facies and stratigraphic architecture of the late-Pleistocene to early-Holocene tide-dominated Paleo-Changjiang(Yangtze River)delta. Geological Society of America Bulletin, 130(3-4): 455-483., articleTitle=Facies and stratigraphic architecture of the late-Pleistocene to early-Holocene tide-dominated Paleo-Changjiang(Yangtze River)delta, refAbstract=null)], funds=[Fund(id=1309196923588936395, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, awardId=C4-24013, language=EN, fundingSource=“Detailed study on the conglomerate reservoir of the Triassic Lower Karamay Formation from Xia 77 area in northwest margin of Junggar Basin”(C4-24013), fundOrder=null, country=null), Fund(id=1309196923656045260, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, awardId=C4-24013, language=CN, fundingSource=*“准噶尔盆地西北缘夏77区块三叠系克下组砾岩储层精细研究”项目(C4-24013), fundOrder=null, country=null)], companyList=[AuthorCompany(id=1309196914239832681, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, xref=null, ext=[AuthorCompanyExt(id=1309196914248221290, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, companyId=1309196914239832681, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=1 PetroChina Xinjiang Oilfield Company,Xinjiang Karamay 834000,China), AuthorCompanyExt(id=1309196914256609899, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, companyId=1309196914239832681, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=1 中国石油新疆油田分公司,新疆克拉玛依 834000)]), AuthorCompany(id=1309196914474713708, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, xref=null, ext=[AuthorCompanyExt(id=1309196914491490925, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, companyId=1309196914474713708, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=2 School of Earth Sciences and Engineering,Nanjing University,Nanjing 210023,China), AuthorCompanyExt(id=1309196914499879534, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, companyId=1309196914474713708, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=2 南京大学地球科学与工程学院,江苏南京 210023)])], figs=[ArticleFig(id=1309196921051382443, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=EN, label=Fig.1, caption=Geographical position of Xia 77 area and northwest margin of Junggar Basin, figureFileSmall=pj0Jc9Ltewv2PBHuPCTyxA==, figureFileBig=FHoRaukDuUfgnx8yvzLiWQ==, tableContent=null), ArticleFig(id=1309196921110102700, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=CN, label=图 1, caption=准噶尔盆地西北缘及夏77地区区域地质背景

a—准噶尔盆地西北缘及玛湖凹陷构造位置; b—夏77地区区域地质背景

, figureFileSmall=pj0Jc9Ltewv2PBHuPCTyxA==, figureFileBig=FHoRaukDuUfgnx8yvzLiWQ==, tableContent=null), ArticleFig(id=1309196921290457773, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=EN, label=Fig.2, caption=Stratigraphic column of the Triassic Lower Karamay Formation of Xia 77 area in northwest margin of Junggar Basin, figureFileSmall=oPNbQ+fUuVsK2U5GeYlLpg==, figureFileBig=9qScgBg9abE04PDjx6Jn3w==, tableContent=null), ArticleFig(id=1309196921361760942, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=CN, label=图 2, caption=准噶尔盆地西北缘夏77地区三叠系克下组地层柱状图, figureFileSmall=oPNbQ+fUuVsK2U5GeYlLpg==, figureFileBig=9qScgBg9abE04PDjx6Jn3w==, tableContent=null), ArticleFig(id=1309196921437258415, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=EN, label=Fig.3, caption=Seismic profile characteristics of Xia 77 area in northwest margin of Junggar Basin, figureFileSmall=tV2yjGaTcrz6LEMcWJUVmw==, figureFileBig=CH+lQd4fXzGCSjVtnlYLSQ==, tableContent=null), ArticleFig(id=1309196921500172976, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=CN, label=图 3, caption=准噶尔盆地西北缘夏77地区地震剖面特征, figureFileSmall=tV2yjGaTcrz6LEMcWJUVmw==, figureFileBig=CH+lQd4fXzGCSjVtnlYLSQ==, tableContent=null), ArticleFig(id=1309196921575670449, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=EN, label=Fig.4, caption=Lithologic content in different conglomerate sections of the Triassic Lower Karamay Formation of Well Xia 042 in northwest margin of Junggar Basin, figureFileSmall=1jIzuImDG0fWy0QUeJwHUQ==, figureFileBig=pvgaRDsYrG4JRKJnEcTZxQ==, tableContent=null), ArticleFig(id=1309196921638585010, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=CN, label=图 4, caption=准噶尔盆地西北缘夏042井克下组不同砾岩层段岩性含量百分比

1—粗—中砾岩; 2—中砾岩; 3— 细—中砾岩; 4—含砂中砾岩; 5—中—细砾岩; 6—细砾岩; 7—砂砾岩; 8—砂岩; 9—泥岩

, figureFileSmall=1jIzuImDG0fWy0QUeJwHUQ==, figureFileBig=pvgaRDsYrG4JRKJnEcTZxQ==, tableContent=null), ArticleFig(id=1309196921701499571, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=EN, label=Fig.5, caption=Sedimentary characteristics of fan delta plain subfacies of the Triassic Lower Karamay Formation of Well Xia 042 in northwest margin of Junggar Basin, figureFileSmall=FAYE16+nLDxLPsJd4PGJPA==, figureFileBig=5oKWT+7pOc4pBbJ4l6ZMQQ==, tableContent=null), ArticleFig(id=1309196921772802740, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=CN, label=图 5, caption=准噶尔盆地西北缘夏042井克下组扇三角洲平原沉积特征, figureFileSmall=FAYE16+nLDxLPsJd4PGJPA==, figureFileBig=5oKWT+7pOc4pBbJ4l6ZMQQ==, tableContent=null), ArticleFig(id=1309196921852494517, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=EN, label=Fig.6, caption=Typical characteristics of core section of the fan delta plain and inner front subfacies of Well Xia 042 in northwest margin of Junggar Basin, figureFileSmall=bgc+Fs2PpTQJrHfnwOESig==, figureFileBig=lMxcoOLRGUAXNlEkOBOz7w==, tableContent=null), ArticleFig(id=1309196921932186294, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=CN, label=图 6, caption=准噶尔盆地西北缘夏042井扇三角洲平原和内前缘岩心典型沉积现象

a—杂色中砾岩,砾石次圆—次棱角状,颗粒支撑,杂乱堆积,1944.55~1944.74 m,T₂ k_1^{2-2},平原辫状河道; b—杂色细—中砾岩,砾石次圆—次棱角状,多级颗粒支撑,杂乱堆积,1945.59~1945.78 m,T₂ k_1^{2-2},平原辫状河道; c—杂色细—中砾岩,砾石次圆—次棱角状,砾石大小不一,砂质杂基—多级颗粒支撑,杂乱堆积,1981.36~1981.44 m,T₂ k_1^3,平原辫状河道; d—杂色中砾岩,含泥砾,次棱角为主,砂质杂基—颗粒支撑,杂乱堆积,1944.89 m,T₂ k_1^{2-2},平原辫状河道; e—青灰色含砂中砾岩,次圆—次棱角状,颗粒支撑,1829.45~1829.64 m,T₂ k_1^{2-1},内前缘水下分流河道; f—青色细—中砾岩,次圆—次棱角状,多级颗粒支撑,1834.95~1835.14 m,T₂ k_1^{2-1},内前缘水下分流河道; g—青灰色含砂中砾岩,次圆—次棱角状,砂质杂基—多级颗粒支撑,1902.59~1902.78 m,T₂ k_1^{2-2},内前缘水下分流河道; h—褐色泥岩,含少量砂砾,水平层理发育,1833.82~1834.04 m,T₂ k_1^{2-1},内前缘水下分流间湾; i—从内前缘水下分流间湾褐色泥岩过渡 到内前缘水下分流河道含砂中砾岩,微相之间以冲刷面为界线,1832.17~1832.36 m,T₂ k_1^{2-1}

, figureFileSmall=bgc+Fs2PpTQJrHfnwOESig==, figureFileBig=lMxcoOLRGUAXNlEkOBOz7w==, tableContent=null), ArticleFig(id=1309196922037043895, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=EN, label=Fig.7, caption=Sedimentary characteristics of the fan delta inner front subfacies of Well Xia 042 in northwest margin of Junggar Basin, figureFileSmall=rA08LGmIhR6uVdXAy6EYoQ==, figureFileBig=CEuW/R+OaE5e2q77c9WvwQ==, tableContent=null), ArticleFig(id=1309196922091569848, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=CN, label=图 7, caption=准噶尔盆地西北缘夏042井扇三角洲内前缘沉积特征, figureFileSmall=rA08LGmIhR6uVdXAy6EYoQ==, figureFileBig=CEuW/R+OaE5e2q77c9WvwQ==, tableContent=null), ArticleFig(id=1309196922188038841, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=EN, label=Fig.8, caption=Characteristics of granularity probability accumulation curves and frequency distribution curves of fan delta front reservoir of Well Xia 042 in northwest margin of Junggar Basin, figureFileSmall=CqtatXYmZEzPsmtk04cuyg==, figureFileBig=E+osofI1t0hyrCYyxWSKzQ==, tableContent=null), ArticleFig(id=1309196922292896442, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=CN, label=图 8, caption=准噶尔盆地西北缘夏042井扇三角洲前缘储集层粒度概率累积曲线和频率分布曲线特征, figureFileSmall=CqtatXYmZEzPsmtk04cuyg==, figureFileBig=E+osofI1t0hyrCYyxWSKzQ==, tableContent=null), ArticleFig(id=1309196922360005307, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=EN, label=Fig.9, caption=Typical characteristics of core section of the fan delta outer front subfacies of Well Xia 042 in northwest margin of Junggar Basin, figureFileSmall=mFLA+oOYEk45AiVEjndv2A==, figureFileBig=6OpD4ffBhOVchp8toErzmA==, tableContent=null), ArticleFig(id=1309196922427114172, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=CN, label=图 9, caption=准噶尔盆地西北缘夏042井扇三角洲外前缘岩心典型沉积现象

a—灰色中砾岩,次棱角—次圆状,逆粒序递变层理,砾石定向排列,颗粒支撑,1972.13~1972.40 m,T₂ k_1^3,外前缘水下分流河道; b—浅灰、青灰色细—中砾岩,次圆为主,砾石定向排列,多级颗粒支撑,1865.09~1865.32 m,T₂ k_1^{2-1},外前缘水下分流河道; c—青灰色细—中砾岩,次棱角—次圆状,多级颗粒支撑,1956.56~1956.79 m,T₂ k_1^3,外前缘水下分流河道; d—杂色中砾岩,次棱角—次圆状,砂质杂基—多级颗粒支撑,1900.03~1900.26 m,T₂ k_1^{2-2},外前缘水下分流河道; e—棕褐色泥岩,水平层理,1953.01~1953.24 m,T₂ k_1^3,外前缘水下分流间湾; f—浅灰、灰色中砂岩、细砂岩和粉砂岩,平行层理和块状层理发育,1953.90~1954.13 m,T₂ k_1^3,外前缘河口坝; g—自下而上从外前缘河口坝灰色含砾粗砂岩过渡到外前缘水下分流河道细—中砾岩,微相之间以冲刷面为界线,界线深度约在1954.72 m,河口坝含砾粗砂岩呈现出逆粒序递变层理,T₂ k_1^3;h—自下而上浅灰色含砾粗砂岩、中砂岩、细砂岩和粉砂岩,呈现出正粒序递变层理,也见平行 层理,1955.34~1955.49 m,T₂ k_1^3,外前缘河口坝

, figureFileSmall=mFLA+oOYEk45AiVEjndv2A==, figureFileBig=6OpD4ffBhOVchp8toErzmA==, tableContent=null), ArticleFig(id=1309196922490028733, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=EN, label=Fig.10, caption=Sedimentary characteristics of the fan delta outer front subfacies of Well Xia 042 in northwest margin of Junggar Basin, figureFileSmall=1cHcBn9sWhmlRCZ8DnV15w==, figureFileBig=GVCZtYli1/zYrQ+b8I1h2A==, tableContent=null), ArticleFig(id=1309196922561331902, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=CN, label=图 10, caption=准噶尔盆地西北缘夏042井扇三角洲外前缘沉积特征, figureFileSmall=1cHcBn9sWhmlRCZ8DnV15w==, figureFileBig=GVCZtYli1/zYrQ+b8I1h2A==, tableContent=null), ArticleFig(id=1309196922628440767, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=EN, label=Fig.11, caption=Sedimentary facies profile of connecting wells in the direction of provenance of Xia 77 area in northwest margin of Junggar Basin, figureFileSmall=W4klWhfXbMS5Gu3a5JzAwQ==, figureFileBig=+C40I8UhPhZJBrNMUdN+HQ==, tableContent=null), ArticleFig(id=1309196922699743936, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=CN, label=图 11, caption=准噶尔盆地西北缘夏77地区顺主物源方向沉积相剖面图, figureFileSmall=W4klWhfXbMS5Gu3a5JzAwQ==, figureFileBig=+C40I8UhPhZJBrNMUdN+HQ==, tableContent=null), ArticleFig(id=1309196922775241409, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=EN, label=Fig.12, caption=Sedimentary facies distribution of the Triassic Lower Karamay Formation of Xia 77 area in northwest margin of Junggar Basin

a—T₂ k_1^3;b—T₂ k_1^{2-2};c—T₂ k_1^{2-1};d—T₂ k_1^1

, figureFileSmall=XBMMWl29nP6JNzsAFGKvkQ==, figureFileBig=ljE43hlmQrMUwLu8DD454w==, tableContent=null), ArticleFig(id=1309196922846544578, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=CN, label=图 12, caption=准噶尔盆地西北缘夏77地区克下组沉积相平面分布, figureFileSmall=XBMMWl29nP6JNzsAFGKvkQ==, figureFileBig=ljE43hlmQrMUwLu8DD454w==, tableContent=null), ArticleFig(id=1309196922922042051, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=EN, label=Table 1, caption=

Stratigraphic division of the Triassic of Xia 77 area in northwest margin of Junggar Basin

, figureFileSmall=null, figureFileBig=null, tableContent=

组		砾岩层段		厚度/m	岩性	与下伏地层接触关系
白碱滩组		—		0~190	厚层状灰色、深灰色泥岩	整合
克拉玛依组	克上组(T2k2)	—		0~300	砾岩、砂岩、泥岩	整合
	克下组(T2k1)	T2 k_1^1		47.0~86.0/59.4	砾岩、砂岩	整合
		T2 k_1^2	T2 k_1^{2-1}	46.0~65.0/60.5	砾岩、砂岩、少量泥岩
			T2 k_1^{2-2}	47.0~67.0/56.9	砾岩、砂岩
		T2 k_1^3		61.0~92.0/71.2	砾岩、砂岩、少量泥岩
百口泉组		—		100~189	棕色砂质泥岩、泥质细砾岩及砂砾岩	不整合

), ArticleFig(id=1309196923001733828, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=CN, label=表 1, caption=

准噶尔盆地西北缘夏77地区三叠系地层划分

, figureFileSmall=null, figureFileBig=null, tableContent=

组		砾岩层段		厚度/m	岩性	与下伏地层接触关系
白碱滩组		—		0~190	厚层状灰色、深灰色泥岩	整合
克拉玛依组	克上组(T2k2)	—		0~300	砾岩、砂岩、泥岩	整合
	克下组(T2k1)	T2 k_1^1		47.0~86.0/59.4	砾岩、砂岩	整合
		T2 k_1^2	T2 k_1^{2-1}	46.0~65.0/60.5	砾岩、砂岩、少量泥岩
			T2 k_1^{2-2}	47.0~67.0/56.9	砾岩、砂岩
		T2 k_1^3		61.0~92.0/71.2	砾岩、砂岩、少量泥岩
百口泉组		—		100~189	棕色砂质泥岩、泥质细砾岩及砂砾岩	不整合

), ArticleFig(id=1309196923098202821, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=EN, label=Table 2, caption=

Thickness and percentage of rock in different conglomerate section of the Triassic Lower Karamay Formation of Well Xia 042 in northwest margin of Junggar Basin

, figureFileSmall=null, figureFileBig=null, tableContent=

岩石类型		地层厚度/m					厚度百分比/%
		T2 k_1^1	T2 k_1^{2-1}	T2 k_1^{2-2}	T2 k_1^3	累计厚度
砾岩	粗—中砾岩	3.30	3.86	0.50	1.68	9.34	4.91	91.96
	中砾岩	6.14	14.79	31.48	21.65	74.06	38.90
	细—中砾岩	1.07	14.31	13.02	5.46	33.86	17.78
	含砂中砾岩	3.13	6.73	15.85	6.63	32.34	16.99
	中—细砾岩	0.00	14.31	4.63	0.29	19.23	10.10
	细砾岩	0.00	0.33	1.31	0.86	2.50	1.31
	砂砾岩	0.00	0.54	2.75	0.47	3.76	1.97
砂岩		2.51	2.91	3.67	3.48	12.57	6.60
泥岩		0.00	2.00	0.00	0.74	2.74	1.44

), ArticleFig(id=1309196923182088902, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=CN, label=表 2, caption=

准噶尔盆地西北缘夏042井T₂k₁不同砾岩层段岩石厚度及其百分比

, figureFileSmall=null, figureFileBig=null, tableContent=

岩石类型		地层厚度/m					厚度百分比/%
		T2 k_1^1	T2 k_1^{2-1}	T2 k_1^{2-2}	T2 k_1^3	累计厚度
砾岩	粗—中砾岩	3.30	3.86	0.50	1.68	9.34	4.91	91.96
	中砾岩	6.14	14.79	31.48	21.65	74.06	38.90
	细—中砾岩	1.07	14.31	13.02	5.46	33.86	17.78
	含砂中砾岩	3.13	6.73	15.85	6.63	32.34	16.99
	中—细砾岩	0.00	14.31	4.63	0.29	19.23	10.10
	细砾岩	0.00	0.33	1.31	0.86	2.50	1.31
	砂砾岩	0.00	0.54	2.75	0.47	3.76	1.97
砂岩		2.51	2.91	3.67	3.48	12.57	6.60
泥岩		0.00	2.00	0.00	0.74	2.74	1.44

), ArticleFig(id=1309196923270169287, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=EN, label=Table 3, caption=

Sedimentary facies of the Triassic Lower Karamay Formation of Xia 77 area in northwest margin of Junggar Basin

, figureFileSmall=null, figureFileBig=null, tableContent=

沉积相	沉积亚相		沉积微相
扇三角洲	扇三角洲平原		辫状河道
			漫滩
			碎屑流带
	扇三角洲前缘	内前缘	水下分流河道
			水下分流间湾
		外前缘	水下分流河道
			水下分流间湾
			河口坝
	前扇三角洲		前扇三角洲泥

), ArticleFig(id=1309196923337278152, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=CN, label=表 3, caption=

准噶尔盆地西北缘夏77地区三叠系克下组沉积相类型

, figureFileSmall=null, figureFileBig=null, tableContent=

沉积相	沉积亚相		沉积微相
扇三角洲	扇三角洲平原		辫状河道
			漫滩
			碎屑流带
	扇三角洲前缘	内前缘	水下分流河道
			水下分流间湾
		外前缘	水下分流河道
			水下分流间湾
			河口坝
	前扇三角洲		前扇三角洲泥

), ArticleFig(id=1309196923408581321, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=EN, label=Table 4, caption=

Sedimentary characteristics of fan delta of the Triassic Lower Karamay Formation of Xia 77 area in northwest margin of Junggar Basin

, figureFileSmall=null, figureFileBig=null, tableContent=

沉积亚相	沉积微相	岩石学特征	沉积构造	测井曲线特征
平原	辫状河道	褐色或杂色粗—中砾岩、中砾岩,砾石分选差,呈次圆—次棱角状,砾石杂乱堆积,呈颗粒支撑、多级颗粒支撑、杂基—多级颗粒支撑和杂基—颗粒支撑	厚层块状构造,砾岩呈片状或舌状,底部见明显的冲刷构造和泥砾	较低的自然电位、自然伽马和声波时差,电阻率曲线呈中—高幅钟形或齿形
	漫滩	辫状河道之间未能沉积砂体的地带,发育褐色泥岩、粉砂质泥岩	水平层理发育	高自然电位、自然伽马和声波时差,低电阻率,电阻率曲线呈齿化漏斗形
	碎屑流带	洪水初期的碎屑流体沿着峡谷进入扇体中上部的沟槽或扇面之上堆积形成。沉积物主要由砾岩构成,砾石含量在60%~90%之间,分选差,常呈不接触状分布在填隙物中,填隙物为不等粒砂级颗粒及泥质	块状构造,砾岩呈舌状,底部见明显的冲刷构造	高自然伽马、中高电阻率和较低声波时差,曲线总体呈现平直形
内前缘	水下分 流河道	浅灰、青灰、青和灰色中砾岩、细—中砾岩、含砂中砾岩,砾石分选较差,磨圆度为次棱角—次圆状,砾石呈颗粒支撑、多级颗粒支撑和杂基—多级颗粒支撑	砾岩底部见明显的冲刷构造和泥砾。砾径向上变小,具弱定向性和递变层理	低自然电位和自然伽马,较低声波时差,电阻率曲线通常呈中—高幅的齿化箱形或钟形,有时呈齿形
	水下分 流间湾	褐色泥岩,含少量粉砂、细砂和细砾	水平层理发育	较高的自然电位、自然伽马和声波时差,电阻率曲线呈低幅的箱形
外前缘	水下分 流河道	灰色或灰绿色中砾岩、细砾岩,分选磨圆中等。砾石呈颗粒支撑、多级颗粒支撑、杂基—多级颗粒支撑和杂基支撑	砾石定向排列	低自然电位和声波时差,自然伽马曲线呈中—高幅的钟形,电阻率曲线通常呈高幅的齿化箱形或钟形
	水下分 流间湾	棕褐色、灰色泥岩或粉砂质泥岩,具纹层结构	水平层理发育	高自然电位、自然伽马和声波时差,低电阻率,电阻率曲线呈齿化漏斗形
	河口坝	细砂—粗砂岩,砾石呈漂浮状具有弱定向性	发育递变、块状和平行层理,以及多期冲刷面和泥砾	较高的自然电位、自然伽马和声波时差,较低电阻率,电阻率曲线呈小幅箱形
前扇三角洲	前扇三 角洲泥	浅灰色泥岩为主,偶见薄层棕色泥岩,夹少量粉砂岩条带或砂质团块	水平层理发育,偶有波状层理、透镜状层理	自然电位曲线平直,电阻率曲线呈低值的小齿状

), ArticleFig(id=1309196923479884490, tenantId=1146029695717560320, journalId=1308397449582313577, articleId=1309196910112637518, language=CN, label=表 4, caption=

准噶尔盆地西北缘夏77地区三叠系克下组扇三角洲沉积特征

, figureFileSmall=null, figureFileBig=null, tableContent=

沉积亚相	沉积微相	岩石学特征	沉积构造	测井曲线特征
平原	辫状河道	褐色或杂色粗—中砾岩、中砾岩,砾石分选差,呈次圆—次棱角状,砾石杂乱堆积,呈颗粒支撑、多级颗粒支撑、杂基—多级颗粒支撑和杂基—颗粒支撑	厚层块状构造,砾岩呈片状或舌状,底部见明显的冲刷构造和泥砾	较低的自然电位、自然伽马和声波时差,电阻率曲线呈中—高幅钟形或齿形
	漫滩	辫状河道之间未能沉积砂体的地带,发育褐色泥岩、粉砂质泥岩	水平层理发育	高自然电位、自然伽马和声波时差,低电阻率,电阻率曲线呈齿化漏斗形
	碎屑流带	洪水初期的碎屑流体沿着峡谷进入扇体中上部的沟槽或扇面之上堆积形成。沉积物主要由砾岩构成,砾石含量在60%~90%之间,分选差,常呈不接触状分布在填隙物中,填隙物为不等粒砂级颗粒及泥质	块状构造,砾岩呈舌状,底部见明显的冲刷构造	高自然伽马、中高电阻率和较低声波时差,曲线总体呈现平直形
内前缘	水下分 流河道	浅灰、青灰、青和灰色中砾岩、细—中砾岩、含砂中砾岩,砾石分选较差,磨圆度为次棱角—次圆状,砾石呈颗粒支撑、多级颗粒支撑和杂基—多级颗粒支撑	砾岩底部见明显的冲刷构造和泥砾。砾径向上变小,具弱定向性和递变层理	低自然电位和自然伽马,较低声波时差,电阻率曲线通常呈中—高幅的齿化箱形或钟形,有时呈齿形
	水下分 流间湾	褐色泥岩,含少量粉砂、细砂和细砾	水平层理发育	较高的自然电位、自然伽马和声波时差,电阻率曲线呈低幅的箱形
外前缘	水下分 流河道	灰色或灰绿色中砾岩、细砾岩,分选磨圆中等。砾石呈颗粒支撑、多级颗粒支撑、杂基—多级颗粒支撑和杂基支撑	砾石定向排列	低自然电位和声波时差,自然伽马曲线呈中—高幅的钟形,电阻率曲线通常呈高幅的齿化箱形或钟形
	水下分 流间湾	棕褐色、灰色泥岩或粉砂质泥岩,具纹层结构	水平层理发育	高自然电位、自然伽马和声波时差,低电阻率,电阻率曲线呈齿化漏斗形
	河口坝	细砂—粗砂岩,砾石呈漂浮状具有弱定向性	发育递变、块状和平行层理,以及多期冲刷面和泥砾	较高的自然电位、自然伽马和声波时差,较低电阻率,电阻率曲线呈小幅箱形
前扇三角洲	前扇三 角洲泥	浅灰色泥岩为主,偶见薄层棕色泥岩,夹少量粉砂岩条带或砂质团块	水平层理发育,偶有波状层理、透镜状层理	自然电位曲线平直,电阻率曲线呈低值的小齿状

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