Article(id=1322942223838486919, tenantId=1146029695717560320, journalId=1322258508890079423, issueId=1322941718441623734, articleNumber=null, orderNo=null, doi=10.13809/j.cnki.cn32-1825/te.2024372, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=null, receivedDate=1735488000000, receivedDateStr=2024-12-30, revisedDate=null, revisedDateStr=null, acceptedDate=null, acceptedDateStr=null, onlineDate=1793343605240, onlineDateStr=2026-10-30, pubDate=1779724800000, pubDateStr=2026-05-26, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1793343605240, onlineIssueDateStr=2026-10-30, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1793343605240, creator=13701087609, updateTime=1793343605240, updator=13701087609, issue=Issue{id=1322941718441623734, tenantId=1146029695717560320, journalId=1322258508890079423, year='2026', volume='16', issue='3', pageStart='489', pageEnd='736', issueExtLink='null', onlineDate='null', pubDate='1779724800000', pubDateStr='2026-05-26', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=1, issueType=-1, specialIssue=null, createTime=1793343484745, creator='13701087609', updateTime=1793344165564, updator='13701087609', preIssue=null, nextIssue=null, articleTotal=null, ext={EN=IssueExt(id=1322944574066402279, tenantId=1146029695717560320, journalId=1322258508890079423, issueId=1322941718441623734, language=EN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=), CN=IssueExt(id=1322944574070596584, tenantId=1146029695717560320, journalId=1322258508890079423, issueId=1322941718441623734, language=CN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=)}, issueFiles=null, downloadFileDto=null}, startPage=583, endPage=596, ext={EN=ArticleExt(id=1322942224060785032, articleId=1322942223838486919, tenantId=1146029695717560320, journalId=1322258508890079423, language=EN, title=Reservoir characteristics and influencing factors of shale oil in second member of Funing Formation, Gaoyou Sag, Subei Basin, columnId=1322941494130258079, journalTitle=Petroleum Reservoir Evaluation and Development, columnName=Oil and Gas Exploration, runingTitle=null, highlight=
The second member of the Paleogene Funing Formation in the Gaoyou Sag, Subei Basin, is one of the key strata for shale oil exploration. Shale reservoir characteristics are important factors influencing oil and gas accumulation, seepage, and migration. To investigate the reservoir characteristics, methods including core observation, X-ray diffraction mineral analysis, N₂ adsorption, scanning electron microscopy, and nuclear magnetic resonance were utilized to study the “four properties” (oil-bearing potential, storage capacity, mobility, and fracturability) of different lithofacies, characterize the reservoir features, and analyze their influencing factors. The results indicated that eight main lithofacies types (Type 1 to Type 8) and four lamination types (felsic lamination, argillaceous lamination, carbonate lamination, and mixed lamination) developed in the study area. The dominant lithofacies were medium-carbon laminated felsic-argillaceous mixed shale, medium-carbon laminated felsic-carbonate mixed shale, and medium-carbon laminated carbonate rock, which were mainly developed in the middle-lower part of sub-member III, sub-member IV, and the middle-lower parts of sub-member V. The storage spaces included pores and fractures. The pores were mainly intergranular (interparticle) pores, while the fractures were mainly tectonic shear fractures, tension-shear fractures, and non-tectonic bedding fractures. The shale reservoirs were influenced by mineral composition, lamination development, and fracture effectiveness. Specifically, intergranular pores in carbonate minerals were relatively small. Higher contents of felsic and argillaceous minerals led to more developed pores and a larger proportion of meso- and macropores. Furthermore, the more uniform the mineral composition of the shale, the better the pore connectivity. Laminated shale exhibited better porosity and permeability, oil-bearing potential, and mobility than other structural types of shale. Unfilled large tectonic shear fractures, bedding fractures, bedding calcite veins, and intralaminar tension-shear fractures constituted effective storage spaces. After fracturing, these could connect pores, forming a complex pore-fracture system. These findings provide support for the evaluation and "sweet spot" selection of shale oil reservoirs in the second member of the Funing Formation, Gaoyou Sag, Subei Basin.
, articleAbstract=null, authors=QIAN FU1, HONGLIANG DUAN1
, 2, WEI CHEN1, YAXIONG SUN1
, 2, SHILI LIU1
, 2, YAN YANG1
, 2, BAOLIANG YANG1
, 3, JINFENG ZHOU1, QIUQIU ZHU1, ZHIMIN LIU1, authorsList=QIAN FU, HONGLIANG DUAN, WEI CHEN, YAXIONG SUN, SHILI LIU, YAN YANG, BAOLIANG YANG, JINFENG ZHOU, QIUQIU ZHU, ZHIMIN LIU, authorCompany=null, correspAuthors=WEI CHEN, authorNote=null, correspAuthorsNote=null, 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=1322942232000602534, articleId=1322942223838486919, tenantId=1146029695717560320, journalId=1322258508890079423, language=CN, title=苏北盆地高邮凹陷阜宁组二段页岩油储层特征及影响因素, columnId=1322941494327390371, journalTitle=油气藏评价与开发, columnName=油气勘探, runingTitle=null, highlight=
苏北盆地高邮凹陷古近系阜宁组二段(以下简称阜二段)是页岩油勘探的重点层系之一,页岩储层特征是影响油气储集、渗流和运移的重要因素,为研究其储层特征,利用岩心观察、X衍射矿物分析、N2吸附、扫描电镜、核磁共振等方法,开展不同岩相“四性”研究,刻画储层特征,分析其影响因素。结果表明:研究区发育8种(①型—⑧型)主要岩相类型和长英质纹层、黏土质纹层、碳酸盐质纹层及混合质纹层4种纹层类型,中碳纹层状长英质-黏土质混合质页岩型、中碳纹层状长英质-碳酸盐质混合质页岩型以及中碳纹层状碳酸盐岩型为优势岩相类型,主要发育在Ⅲ亚段中下部、Ⅳ亚段以及Ⅴ亚段中下部,储集空间包括孔隙和裂缝,孔隙以粒间(缘)孔为主,裂缝以构造剪切缝、张剪缝和非构造层理缝为主。页岩储层受矿物组分、纹层发育程度和裂缝有效性影响,碳酸盐岩矿物粒间孔相对较小,长英质和黏土质矿物含量越高,孔隙越发育,中大孔占比越大,页岩矿物组分越单一,孔隙连通性越好。纹层状页岩孔渗、含油性及可动性优于其他构造类型页岩。未被充填的大型构造剪切缝、层理缝、顺层方解石脉和层内张剪缝为有效储集空间,压裂后可沟通孔隙,形成复杂孔-缝系统。研究成果为苏北盆地高邮凹陷阜二段页岩油储层评价和“甜点”优选提供支撑。
, articleAbstract=null, authors=付茜1, 段宏亮1
, 2, 陈伟1, 孙雅雄1
, 2, 刘世丽1
, 2, 杨艳1
, 2, 杨保良1
, 3, 周进峰1, 朱秋秋1, 刘志敏1, authorsList=付茜, 段宏亮, 陈伟, 孙雅雄, 刘世丽, 杨艳, 杨保良, 周进峰, 朱秋秋, 刘志敏, authorCompany=null, correspAuthors=陈伟, authorNote=
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付茜(1991—),女,硕士研究生,副研究员,主要从事油气勘探研究工作。地址:江苏省扬州市文汇西路1号江苏油田分公司,邮政编码:225009。E-mail:fuq.jsyt@sinopec.com
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付茜(1991—),女,硕士研究生,副研究员,主要从事油气勘探研究工作。地址:江苏省扬州市文汇西路1号江苏油田分公司,邮政编码:225009。E-mail:fuq.jsyt@sinopec.com
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1 Sinopec Jiangsu Oilfield Company, Yangzhou, Jiangsu 225009, China
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1 中国石化江苏油田分公司,江苏 扬州 225009
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1 中国石化江苏油田分公司,江苏 扬州 225009)]), AuthorCompany(id=1322942232399061418, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, xref=2, ext=[AuthorCompanyExt(id=1322942232407450027, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, companyId=1322942232399061418, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=
2 State Key Laboratory of Shale Oil and Gas Enrichment Mechanisms and Effective Development, Beijing 102206, China), AuthorCompanyExt(id=1322942232415838636, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, companyId=1322942232399061418, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=
2 页岩油气富集机理与高效开发全国重点实验室,北京 102206)])]), Author(id=1322942233078538684, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, orderNo=2, firstName=null, middleName=null, lastName=null, nameCn=null, orcid=null, stid=null, country=null, authorPic=null, dead=0, email=null, emailSecond=null, emailThird=null, correspondingAuthor=1, authorType=1, ext={EN=AuthorExt(id=1322942233170813374, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, authorId=1322942233078538684, language=EN, stringName=WEI CHEN, firstName=WEI, middleName=null, lastName=CHEN, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=1, address=
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1 中国石化江苏油田分公司,江苏 扬州 225009, bio=null, bioImg=null, bioContent=null, aboutCorrespAuthor=null)}, companyList=[AuthorCompany(id=1322942232298398119, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, xref=1, ext=[AuthorCompanyExt(id=1322942232310981032, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, companyId=1322942232298398119, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=
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1 Sinopec Jiangsu Oilfield Company, Yangzhou, Jiangsu 225009, China
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1 中国石化江苏油田分公司,江苏 扬州 225009
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2 State Key Laboratory of Shale Oil and Gas Enrichment Mechanisms and Effective Development, Beijing 102206, China), AuthorCompanyExt(id=1322942232415838636, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, companyId=1322942232399061418, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=
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1 Sinopec Jiangsu Oilfield Company, Yangzhou, Jiangsu 225009, China
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1 中国石化江苏油田分公司,江苏 扬州 225009
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1 Sinopec Jiangsu Oilfield Company, Yangzhou, Jiangsu 225009, China), AuthorCompanyExt(id=1322942232319369641, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, companyId=1322942232298398119, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=
1 中国石化江苏油田分公司,江苏 扬州 225009)]), AuthorCompany(id=1322942232399061418, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, xref=2, ext=[AuthorCompanyExt(id=1322942232407450027, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, companyId=1322942232399061418, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=
2 State Key Laboratory of Shale Oil and Gas Enrichment Mechanisms and Effective Development, Beijing 102206, China), AuthorCompanyExt(id=1322942232415838636, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, companyId=1322942232399061418, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=
2 页岩油气富集机理与高效开发全国重点实验室,北京 102206)]), AuthorCompany(id=1322942232508113325, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, xref=3, ext=[AuthorCompanyExt(id=1322942232520696238, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, companyId=1322942232508113325, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=
3 School of Ocean and Earth Science, Tongji University, Shanghai 200092, China), AuthorCompanyExt(id=1322942232533279151, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, companyId=1322942232508113325, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=
3 同济大学海洋与地球科学学院,上海 200092)])], figs=[ArticleFig(id=1322942238073954804, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=EN, label=Fig.1, caption=
Distribution of shale oil wells in member 2 of Funing Formation, Gaoyou Sag, Subei Basin(modified from reference[14]), figureFileSmall=611i3Kqb0GzeSmiyOjostg==, figureFileBig=vVgWOURIaRJAjvYky3oCQg==, tableContent=null), ArticleFig(id=1322942238145257973, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=CN, label=图1, caption=
苏北盆地高邮凹陷阜宁组二段页岩油井分布(据文献[14]修改), figureFileSmall=611i3Kqb0GzeSmiyOjostg==, figureFileBig=vVgWOURIaRJAjvYky3oCQg==, tableContent=null), ArticleFig(id=1322942238367556086, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=EN, label=Fig.2, caption=
Comprehensive stratigraphic column of second member of Funing Formation in well HY7, Gaoyou Sag, Subei Basin, figureFileSmall=CJO+x5jnohmqPcpY+5LjPw==, figureFileBig=CqQ7mBbqQj4KgdjBf/O5OQ==, tableContent=null), ArticleFig(id=1322942238438859255, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=CN, label=图2, caption=
苏北盆地高邮凹陷HY7井阜宁组二段综合柱状图注:w(TOC)为总有机碳含量,%;S1为游离烃含量,单位mg/g;Ios为含油饱和度指数,单位mg/g。
, figureFileSmall=CJO+x5jnohmqPcpY+5LjPw==, figureFileBig=CqQ7mBbqQj4KgdjBf/O5OQ==, tableContent=null), ArticleFig(id=1322942238505968120, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=EN, label=Fig.3, caption=
Triangular diagram of shale mineral composition in second member of Funing Formation in well HY7, Gaoyou Sag, Subei Basin, figureFileSmall=RkH4nWK8iPniVeflGWROww==, figureFileBig=9qntCUqLvP0BddBYORNGxQ==, tableContent=null), ArticleFig(id=1322942238615020025, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=CN, label=图3, caption=
苏北盆地高邮凹陷HY7井阜宁组二段页岩矿物组分三角图, figureFileSmall=RkH4nWK8iPniVeflGWROww==, figureFileBig=9qntCUqLvP0BddBYORNGxQ==, tableContent=null), ArticleFig(id=1322942238698906106, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=EN, label=Fig.4, caption=
Thin section and scanning electron microscopy images of different lithofacies in second member of Funing Formation in well HY7, Gaoyou Sag, Subei Basin, figureFileSmall=24L3WpCtZYy86DkPNDF4WA==, figureFileBig=uZcRlhlT8S/aVY18Hahvkg==, tableContent=null), ArticleFig(id=1322942238786986491, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=CN, label=图4, caption=
苏北盆地高邮凹陷HY7井阜宁组二段各岩相薄片和扫描电镜图像, figureFileSmall=24L3WpCtZYy86DkPNDF4WA==, figureFileBig=uZcRlhlT8S/aVY18Hahvkg==, tableContent=null), ArticleFig(id=1322942238862483964, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=EN, label=Fig.5, caption=
Type ① shale pore distribution and morphology, figureFileSmall=UweToNIxaFdV6aqnadHcRQ==, figureFileBig=z3gDigBjbc/X1bXWe2WICw==, tableContent=null), ArticleFig(id=1322942238937981437, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=CN, label=图5, caption=
①型页岩孔隙分布和形态注:NMR⋲×T2为核磁共振线性拟合曲线;NMR⋲k×T2k为核磁共振幂指数拟合曲线。
, figureFileSmall=UweToNIxaFdV6aqnadHcRQ==, figureFileBig=z3gDigBjbc/X1bXWe2WICw==, tableContent=null), ArticleFig(id=1322942240603120126, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=EN, label=Fig.6, caption=
Type ② shale pore distribution and morphology, figureFileSmall=6fMsuxLNWoe0e897ddA5bw==, figureFileBig=/uEYOWLJ+I8WdA6zfcIfig==, tableContent=null), ArticleFig(id=1322942240674423295, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=CN, label=图6, caption=
②型页岩孔隙分布和形态, figureFileSmall=6fMsuxLNWoe0e897ddA5bw==, figureFileBig=/uEYOWLJ+I8WdA6zfcIfig==, tableContent=null), ArticleFig(id=1322942240762503680, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=EN, label=Fig.7, caption=
Type ③ shale pore distribution and morphology, figureFileSmall=TYMWlo4UxPoM8AZ7V0kRog==, figureFileBig=kdwdC7nuLyOUDhoQtuHzyg==, tableContent=null), ArticleFig(id=1322942240829612545, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=CN, label=图7, caption=
③型页岩孔隙分布和形态, figureFileSmall=TYMWlo4UxPoM8AZ7V0kRog==, figureFileBig=kdwdC7nuLyOUDhoQtuHzyg==, tableContent=null), ArticleFig(id=1322942240913498626, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=EN, label=Fig.8, caption=
Type ④ shale pore distribution and morphology, figureFileSmall=zCj8GiVcExUIpnR2YZdnFw==, figureFileBig=gWnyFP7eU5Es47PSorTQsg==, tableContent=null), ArticleFig(id=1322942240988996099, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=CN, label=图8, caption=
④型页岩孔隙分布和形态, figureFileSmall=zCj8GiVcExUIpnR2YZdnFw==, figureFileBig=gWnyFP7eU5Es47PSorTQsg==, tableContent=null), ArticleFig(id=1322942241081270788, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=EN, label=Fig.9, caption=
Type ⑤ shale pore distribution and morphology, figureFileSmall=C7C8ZydFBPsa6Cqr5r2doQ==, figureFileBig=ID7ESpsMGm6c1XEoUYjqWA==, tableContent=null), ArticleFig(id=1322942241160962565, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=CN, label=图9, caption=
⑤型页岩孔隙分布和形态, figureFileSmall=C7C8ZydFBPsa6Cqr5r2doQ==, figureFileBig=ID7ESpsMGm6c1XEoUYjqWA==, tableContent=null), ArticleFig(id=1322942241223877126, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=EN, label=Fig.10, caption=
Type ⑥ shale pore distribution and morphology, figureFileSmall=gy/G0rHQDawJzknk8CoIGA==, figureFileBig=z1DqOXDc/ROT4MTSRBnHnQ==, tableContent=null), ArticleFig(id=1322942241290985991, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=CN, label=图10, caption=
⑥型页岩孔隙分布和形态, figureFileSmall=gy/G0rHQDawJzknk8CoIGA==, figureFileBig=z1DqOXDc/ROT4MTSRBnHnQ==, tableContent=null), ArticleFig(id=1322942241362289160, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=EN, label=Fig.11, caption=
Type ⑦ shale pore distribution and morphology, figureFileSmall=OnKOEipkyUgeIbrvoHETcg==, figureFileBig=LyGvcxf+g0aV7QBkZrcHdg==, tableContent=null), ArticleFig(id=1322942241483923977, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=CN, label=图11, caption=
⑦型页岩孔隙分布和形态, figureFileSmall=OnKOEipkyUgeIbrvoHETcg==, figureFileBig=LyGvcxf+g0aV7QBkZrcHdg==, tableContent=null), ArticleFig(id=1322942241555227146, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=EN, label=Fig.12, caption=
Type ⑧ shale pore distribution and morphology, figureFileSmall=rlNGTdZb37Ea9fWjbpWc2w==, figureFileBig=ts99DiHEjWw0k3+wn3R2sg==, tableContent=null), ArticleFig(id=1322942241626530315, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=CN, label=图12, caption=
⑧型页岩孔隙分布和形态, figureFileSmall=rlNGTdZb37Ea9fWjbpWc2w==, figureFileBig=ts99DiHEjWw0k3+wn3R2sg==, tableContent=null), ArticleFig(id=1322942241693639180, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=EN, label=Fig.13, caption=
Fracture characteristics of cores from second member of Funing Formation in well HY7, Gaoyou Sag, Subei Basin, figureFileSmall=kvuejP2hS0i9iIpzRlewdQ==, figureFileBig=1ieo95RCFAiEJzEkonL4bg==, tableContent=null), ArticleFig(id=1322942241752359437, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=CN, label=图13, caption=
苏北盆地高邮凹陷HY7井阜宁组二段岩心裂缝特征注:a为大型剪切缝,HY7井3 974.2 m;b为树枝状张性缝,HY7井3 987.3 m;c为张性缝,HY7井4 047.54 m;d为白云石条带内张剪缝,HY7井4 146.47 m;e为长英质纹层内张剪缝,HY7井4 040.0 m;f为长英质纹层内张剪缝,HY7井4 142.39 m;g为小断层,HY7井4 149.32 m;h为滑脱缝,HY7井4 021.25 m;i为层理缝,HY7井4 124.0 m;j为层理缝面含油,HY7井4 107.34 m;k为顺层方解石脉,HY7井4 023.68 m;l为顺层方解石脉内溶蚀缝洞,HY7井4 230.19 m;m为粒缘缝,HY7井4 036.1 m。
, figureFileSmall=kvuejP2hS0i9iIpzRlewdQ==, figureFileBig=1ieo95RCFAiEJzEkonL4bg==, tableContent=null), ArticleFig(id=1322942241840439822, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=EN, label=Fig.14, caption=
Relationship between shale mineral composition, sedimentary structures, and reservoir pore characteristics in second member of Funing Formation in well HY7, Gaoyou Sag, Subei Basin, figureFileSmall=Pxr91gj9HJ0si7387uobQg==, figureFileBig=9uclb0LDNGN6vOacCMx2vg==, tableContent=null), ArticleFig(id=1322942241928520207, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=CN, label=图14, caption=
苏北盆地高邮凹陷HY7井阜宁组二段页岩矿物组分、沉积构造与储层孔隙特征关系, figureFileSmall=Pxr91gj9HJ0si7387uobQg==, figureFileBig=9uclb0LDNGN6vOacCMx2vg==, tableContent=null), ArticleFig(id=1322942242041766416, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=EN, label=Table 1, caption=
Comparison of parameters of different lithofacies in second member of Funing Formation in well HY7,Gaoyou Sag,Subei Basin, figureFileSmall=null, figureFileBig=null, tableContent=
| 主要岩相类型 | 含油性 | 可动性 | 储集性 | 可压性 |
|---|
| ω(TOC)/% | 含油饱和度/% | S1/(mg/g) | IOS/(mg/g) | He孔隙度/% | 渗透率/10-3 μm2 | 脆性矿物含量/% |
|---|
| 中碳纹层状长英质-黏土质混合质页岩(①型) | 1.47 | 44.25 | 1.50 | 112 | 1.91 | 1.90 | 60.89 |
| 中碳纹层状长英质-碳酸盐质混合质页岩(②型) | 1.13 | 41.77 | 1.38 | 126 | 2.05 | 1.22 | 73.69 |
| 低碳纹层状/层状长英质-黏土质混合质页岩(③型) | 0.75 | 34.74 | 0.81 | 85 | 1.89 | 3.57 | 61.32 |
| 低碳纹层状/层状长英质-碳酸盐质混合质页岩(④型) | 0.74 | 44.09 | 0.96 | 90 | 1.84 | 2.94 | 74.92 |
| 中/低碳纹层状/层状长英页岩(⑤型) | 0.83 | 37.21 | 0.98 | 118 | 2.42 | 0.43 | 72.59 |
| 中碳纹层状碳酸盐岩(⑥型) | 1.53 | 35.58 | 1.64 | 110 | 1.61 | 1.13 | 88.44 |
| 中碳块状长英质-黏土质混合质页岩(⑦型) | 1.51 | - | 1.19 | 86 | 1.10 | 0.03 | 59.00 |
| 高碳块状长英质-碳酸盐质混合质页岩(⑧型) | 2.31 | - | 1.44 | 62 | 0.98 | 0.01 | 80.50 |
), ArticleFig(id=1322942242134041105, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322942223838486919, language=CN, label=表1, caption=
苏北盆地高邮凹陷HY7井阜宁组二段不同岩相参数对比
, figureFileSmall=null, figureFileBig=null, tableContent=
| 主要岩相类型 | 含油性 | 可动性 | 储集性 | 可压性 |
|---|
| ω(TOC)/% | 含油饱和度/% | S1/(mg/g) | IOS/(mg/g) | He孔隙度/% | 渗透率/10-3 μm2 | 脆性矿物含量/% |
|---|
| 中碳纹层状长英质-黏土质混合质页岩(①型) | 1.47 | 44.25 | 1.50 | 112 | 1.91 | 1.90 | 60.89 |
| 中碳纹层状长英质-碳酸盐质混合质页岩(②型) | 1.13 | 41.77 | 1.38 | 126 | 2.05 | 1.22 | 73.69 |
| 低碳纹层状/层状长英质-黏土质混合质页岩(③型) | 0.75 | 34.74 | 0.81 | 85 | 1.89 | 3.57 | 61.32 |
| 低碳纹层状/层状长英质-碳酸盐质混合质页岩(④型) | 0.74 | 44.09 | 0.96 | 90 | 1.84 | 2.94 | 74.92 |
| 中/低碳纹层状/层状长英页岩(⑤型) | 0.83 | 37.21 | 0.98 | 118 | 2.42 | 0.43 | 72.59 |
| 中碳纹层状碳酸盐岩(⑥型) | 1.53 | 35.58 | 1.64 | 110 | 1.61 | 1.13 | 88.44 |
| 中碳块状长英质-黏土质混合质页岩(⑦型) | 1.51 | - | 1.19 | 86 | 1.10 | 0.03 | 59.00 |
| 高碳块状长英质-碳酸盐质混合质页岩(⑧型) | 2.31 | - | 1.44 | 62 | 0.98 | 0.01 | 80.50 |
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