Article(id=1242134432375714462, tenantId=1146029695717560320, journalId=1146031591421210625, issueId=1242134390566887892, articleNumber=null, orderNo=23, doi=10.3981/j.issn.1000-7857.2016.2.017, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=null, receivedDate=1417449600000, receivedDateStr=2014-12-02, revisedDate=1441814400000, revisedDateStr=2015-09-10, acceptedDate=null, acceptedDateStr=null, onlineDate=1454555982870, onlineDateStr=2016-02-04, pubDate=1453910400000, pubDateStr=2016-01-28, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1454555982870, onlineIssueDateStr=2016-02-04, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1774077526416, creator=sys-migrate, updateTime=1774077526416, updator=sys-migrate, issue=Issue{id=1242134390566887892, tenantId=1146029695717560320, journalId=1146031591421210625, year='2016', volume='34', issue='2', pageStart='1', pageEnd='332', issueExtLink='null', onlineDate='null', pubDate='1453910400000', pubDateStr='2016-01-28', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=3, issueType=-1, specialIssue=null, createTime=1774077516449, creator='sys-migrate', updateTime=1774077516449, updator='sys-migrate', preIssue=null, nextIssue=null, articleTotal=null, ext=null, issueFiles=null, downloadFileDto=null}, startPage=110, endPage=115, ext={EN=ArticleExt(id=1242134438650389178, articleId=1242134432375714462, tenantId=1146029695717560320, journalId=1146031591421210625, language=EN, title=Sedimentary environments and sandbody distribution in member 2 of Permian Shanxi formation in mid-eastern Ordos Basin, columnId=1242116810380743325, journalTitle=Science & Technology Review, columnName=Reviews, runingTitle=null, highlight=null, articleAbstract=The member 2 of Lower Permian Shanxi formation is a main gas-producing reservoir and an important layer for exploration in the mid-eastern Ordos Basin. Outcrop analysis, core observation, comprehensive logging data interpretation and geochemical analysis suggest that the study area was affected by Marine facies at the early-middle stage of member 2 of Shanxi formation. It developed a rivertide controlled delta at the 2 and 3 sub-member of member 2 of Shanxi formation. The delta plain included distributary channel, abandoned channel, peat swamps and interdistributary depression. The delta front included sedimentary micro-facies, such as underwater distributary channel, mouth bar, distal bar, tide sand dam, and interdistributary bay. Seawater pushed out along the southeast Ordos Basin in the age of the 1 sub-member of member 2 of Shanxi formation. The study area developed a river controlled-lake delta on the background of terrestrial lakes. The differences of ancient geographical conditions lead to the different types of sand and reservoir properties. The reservoir sand in the 3 sub-member of member 2 of Shanxi formation was changed by the marine facies completely in the Mizhi-Zizhou and Tawan-Gaoqiao area. It has more advantages in lithologic characteristics, sand thickness and reservoir performance, which are favorable for gas exploration., authors=YANG Wei1,2, WANG Feng1, authorsList=YANG Wei, WANG Feng, authorCompany=1. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China;
2. Engineering Investigation and Design Institute, Sichuan Provincial Coalfield Bureau, Chengdu 610072, China, correspAuthors=null, authorNote=null, correspAuthorsNote=null, copyrightStatement=null, copyrightOwner=null, extLink=null, articleAbsUrl=null, sourceXml=null, magXml=null, pdfUrl=null, pdf=HZbKbU0OmsVn6SNK/KAfoQ==, pdfFileSize=10576905, 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=1242134435236225703, articleId=1242134432375714462, tenantId=1146029695717560320, journalId=1146031591421210625, language=CN, title=鄂尔多斯盆地中东部二叠系山西组2段沉积环境及砂体展布, columnId=1242116809164390686, journalTitle=科技导报, columnName=综述文章, runingTitle=null, highlight=null, articleAbstract=鄂尔多斯盆地中东部下二叠统山西组2 段为重要的勘探层位和主力产气层。在野外露头分析、岩心观察、测井资料综合解释以及地球化学分析的基础上,研究认为山西组2 段早中期研究区受海相作用影响,山32、山22 期发育河控-潮控三角洲,其三角洲平原包括分流河道、废弃河道、泥炭沼泽和分流间洼地,三角洲前缘包括水下分流河道、河口坝、远砂坝、潮汐砂坝、分流间湾等沉积微相;山12期海水沿东南方向推出鄂尔多斯盆地,研究区在陆相湖泊背景上发育河控-湖泊三角洲。古地理条件的不同使其砂体类型及储集性能也有一定的差异,其中米脂-子洲及塔湾-高桥地区山32段储集砂体受海相环境改造彻底,在岩性特征、砂体厚度以及储集性能方面更具优越性,为天然气勘探的有利目标区。, authors=阳伟1,2, 王峰1, authorsList=阳伟, 王峰, authorCompany=1. 成都理工大学沉积地质研究院, 成都 610059;
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鄂尔多斯盆地中东部二叠系山西组2段沉积环境及砂体展布
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阳伟, 王峰
科技导报 | 综述文章 2016,34(2): 110-115
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科技导报 |综述文章 2016 , 34 (2) : 110 -115
鄂尔多斯盆地中东部二叠系山西组2段沉积环境及砂体展布
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阳伟, 王峰
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作者简介:
阳伟,工程师,研究方向为沉积学及岩相古地理,电子信箱:57684830@qq.com
Sedimentary environments and sandbody distribution in member 2 of Permian Shanxi formation in mid-eastern Ordos Basin
YANG Wei, WANG Feng
Affiliations
    1. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China;
    2. Engineering Investigation and Design Institute, Sichuan Provincial Coalfield Bureau, Chengdu 610072, China
出版时间: 2016-01-28 doi: 10.3981/j.issn.1000-7857.2016.2.017
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鄂尔多斯盆地中东部下二叠统山西组2 段为重要的勘探层位和主力产气层。在野外露头分析、岩心观察、测井资料综合解释以及地球化学分析的基础上,研究认为山西组2 段早中期研究区受海相作用影响,山32、山22 期发育河控-潮控三角洲,其三角洲平原包括分流河道、废弃河道、泥炭沼泽和分流间洼地,三角洲前缘包括水下分流河道、河口坝、远砂坝、潮汐砂坝、分流间湾等沉积微相;山12期海水沿东南方向推出鄂尔多斯盆地,研究区在陆相湖泊背景上发育河控-湖泊三角洲。古地理条件的不同使其砂体类型及储集性能也有一定的差异,其中米脂-子洲及塔湾-高桥地区山32段储集砂体受海相环境改造彻底,在岩性特征、砂体厚度以及储集性能方面更具优越性,为天然气勘探的有利目标区。
沉积环境  /  砂体展布  /  山2 段  /  鄂尔多斯盆地
The member 2 of Lower Permian Shanxi formation is a main gas-producing reservoir and an important layer for exploration in the mid-eastern Ordos Basin. Outcrop analysis, core observation, comprehensive logging data interpretation and geochemical analysis suggest that the study area was affected by Marine facies at the early-middle stage of member 2 of Shanxi formation. It developed a rivertide controlled delta at the 2 and 3 sub-member of member 2 of Shanxi formation. The delta plain included distributary channel, abandoned channel, peat swamps and interdistributary depression. The delta front included sedimentary micro-facies, such as underwater distributary channel, mouth bar, distal bar, tide sand dam, and interdistributary bay. Seawater pushed out along the southeast Ordos Basin in the age of the 1 sub-member of member 2 of Shanxi formation. The study area developed a river controlled-lake delta on the background of terrestrial lakes. The differences of ancient geographical conditions lead to the different types of sand and reservoir properties. The reservoir sand in the 3 sub-member of member 2 of Shanxi formation was changed by the marine facies completely in the Mizhi-Zizhou and Tawan-Gaoqiao area. It has more advantages in lithologic characteristics, sand thickness and reservoir performance, which are favorable for gas exploration.
sedimentary environments  /  sand-body distribution  /  member 2 of Shanxi formation  /  Ordos Basin
阳伟, 王峰. 鄂尔多斯盆地中东部二叠系山西组2段沉积环境及砂体展布. 科技导报, 2016 , 34 (2) : 110 -115 . DOI: 10.3981/j.issn.1000-7857.2016.2.017
YANG Wei, WANG Feng. Sedimentary environments and sandbody distribution in member 2 of Permian Shanxi formation in mid-eastern Ordos Basin[J]. Science & Technology Review, 2016 , 34 (2) : 110 -115 . DOI: 10.3981/j.issn.1000-7857.2016.2.017

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doi: 10.3981/j.issn.1000-7857.2016.2.017
  • 接收时间:2014-12-02
  • 首发时间:2016-02-04
  • 出版时间:2016-01-28
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  • 收稿日期:2014-12-02
  • 修回日期:2015-09-10
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2种不同金属材料的力学参数
科
Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)
属
Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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