Article(id=1322941676129497169, tenantId=1146029695717560320, journalId=1322258508890079423, issueId=1322941491332657306, articleNumber=null, orderNo=null, doi=10.13809/j.cnki.cn32-1825/te.20250097, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=null, receivedDate=1766332800000, receivedDateStr=2025-12-22, revisedDate=null, revisedDateStr=null, acceptedDate=null, acceptedDateStr=null, onlineDate=1793343474657, onlineDateStr=2026-10-30, pubDate=1795622400000, pubDateStr=2026-11-26, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1793343474657, onlineIssueDateStr=2026-10-30, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1793343474657, creator=13701087609, updateTime=1793343474657, updator=13701087609, issue=Issue{id=1322941491332657306, tenantId=1146029695717560320, journalId=1322258508890079423, year='2026', volume='16', issue='6', pageStart='1137', pageEnd='1368', issueExtLink='null', onlineDate='null', pubDate='1795622400000', pubDateStr='2026-11-26', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=1, issueType=1, specialIssue=null, createTime=1793343430598, creator='13701087609', updateTime=1793344116766, updator='13701087609', preIssue=null, nextIssue=null, articleTotal=null, ext={EN=IssueExt(id=1322944369447285513, tenantId=1146029695717560320, journalId=1322258508890079423, issueId=1322941491332657306, language=EN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=), CN=IssueExt(id=1322944369447285514, tenantId=1146029695717560320, journalId=1322258508890079423, issueId=1322941491332657306, language=CN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=)}, issueFiles=null, downloadFileDto=null}, startPage=1227, endPage=1239, ext={EN=ArticleExt(id=1322941677941436499, articleId=1322941676129497169, tenantId=1146029695717560320, journalId=1322258508890079423, language=EN, title=Development patterns of natural fractures in continental shale of Fengcheng Formation in Mahu Sag of Junggar Basin: insights from imaging logs, columnId=1322941494130258079, journalTitle=Petroleum Reservoir Evaluation and Development, columnName=Oil and Gas Exploration, runingTitle=null, highlight=

The Lower Permian Fengcheng Formation in the Mahu Sag, Junggar Basin, contains an organic-rich lacustrine shale succession with abundant oil and gas resources. However, deep continental shale reservoirs are generally characterized by low porosity and permeability. Widespread natural fractures play an important role in shale oil enrichment and development, but the limited understanding of natural fracture development patterns in continental shale has hindered the formulation of detailed development strategies for shale reservoirs in the Mahu Sag. In this study, based on microresistivity imaging logs, natural fractures in the Fengcheng Formation of the Mahu Sag were identified in detail. Quantitative characterization was conducted on fracture parameters, including strike, dip angle, aperture, and density. On this basis, the development characteristics, controlling factors, and distribution patterns of natural fractures in the study area were analyzed. The results demonstrated that natural fractures in the Fengcheng Formation shale of the Mahu Sag were predominantly high-angle tectonic fractures, which could be categorized into bed-crossing fractures and interlayer fractures. Their dip angles were mainly concentrated between 60° and 90°, while apertures were dominantly within 0-0.2 mm. High-resistivity fractures accounted for a distinctly dominant proportion. The tectonic were mainly oriented north-northwest-south-southeast (NNW-SSE), approximately east-west (E-W), and north-northeast-south-southwest (NNE-SSW). The development degree of natural fractures in the study area was strongly controlled by mineral composition and the thickness of mechanical stratigraphy. Compared with the first member of the Fengcheng Formation, natural fractures were more developed in the second member, characterized by a high brittle-mineral content, and the third member, which had relatively thinner mechanical stratigraphy. Fracture filling characteristics varied significantly among different strikes. Most fractures trending east-northeast-west-southwest (NEE-SWW) were incompletely mineral-filled, indicating higher effectiveness. In addition, fracture aperture showed a positive correlation with the angle between the fracture dipping direction and the orientation of the maximum horizontal principal stress. Fractures with dip directions nearly parallel to the orientation of the maximum horizontal principal stress exhibited minimal apertures and the lowest effectiveness. Vertically, natural fractures in the first member of the Fengcheng Formation displayed a larger average angle between their dip direction and the maximum horizontal principal stress orientation and correspondingly the highest effectiveness. By contrast, natural fractures in the second member showed a smaller angle and exhibited the lowest effectiveness. These results provide an important geological basis for the detailed evaluation of natural fractures in deep continental shale and the efficient development of shale oil in the Mahu Sag.

, articleAbstract=null, authors=XING ZHANG1, GUOPING LIU1, ZHENLIN WANG2, JIANGLONG YU2, XUAN TANG1, CAIGUANG LIU2, SONG CAO3, SHAOBO GAO1, authorsList=XING ZHANG, GUOPING LIU, ZHENLIN WANG, JIANGLONG YU, XUAN TANG, CAIGUANG LIU, SONG CAO, SHAOBO GAO, authorCompany=null, correspAuthors=GUOPING LIU, 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=1322941680395104358, articleId=1322941676129497169, tenantId=1146029695717560320, journalId=1322258508890079423, language=CN, title=准噶尔盆地玛湖凹陷风城组陆相页岩天然裂缝发育规律：成像测井带来的启示, columnId=1322941494327390371, journalTitle=油气藏评价与开发, columnName=油气勘探, runingTitle=null, highlight=

准噶尔盆地玛湖凹陷下二叠统风城组发育一套富有机质湖相页岩，油气资源丰富，然而，深层陆相页岩储层孔隙度和渗透率普遍较低。广泛发育的天然裂缝在页岩油的富集与开发过程中发挥着重要作用，但对陆相页岩天然裂缝的发育规律认识不足，限制了玛湖凹陷页岩储层的精细化开发方案的制定。本研究基于微电阻率成像测井资料，对玛湖凹陷风城组天然裂缝进行精细化识别，定量表征裂缝走向、倾角、开度及密度等参数，分析研究区天然裂缝发育特征、控制因素及展布规律。研究结果表明：玛湖凹陷风城组页岩中天然裂缝以高角度构造裂缝为主，可划分为穿层裂缝和层内裂缝两类，倾角集中于60°~90°，开度以0~0.2 mm为主，高阻裂缝发育占比具有明显优势，主要发育NNW—SSE（北北西—南南东）向、近E—W（东—西）向、NNE—SSW（北北东—南南西）向的构造裂缝。研究区天然裂缝发育程度受矿物组成和岩石力学层厚度的影响明显，具有高脆性矿物含量的风二段和岩石力学层较薄的风三段的天然裂缝发育程度高于风一段。不同走向裂缝的充填性差异较大，NEE—SWW（北东东—南西西）向走向裂缝多数未被矿物完全充填，有效性较好，且裂缝开度随裂缝倾向与最大水平主应力方向夹角增加而增加。研究区内与最大水平主应力方向近平行的NEE—SWW向倾向裂缝开度最小、有效性最差。垂向上，风一段天然裂缝倾向与最大水平主应力方向平均夹角较大，有效性最好；风二段天然裂缝倾向与最大水平主应力方向平均夹角较小，有效性最差。研究成果为深层陆相页岩天然裂缝的精细评价和玛湖凹陷页岩油高效开发提供了重要地质依据。

, articleAbstract=null, authors=张星1, 刘国平1, 王振林2, 于江龙2, 唐玄1, 刘财广2, 曹嵩3, 高少博1, authorsList=张星, 刘国平, 王振林, 于江龙, 唐玄, 刘财广, 曹嵩, 高少博, authorCompany=null, correspAuthors=刘国平, authorNote=, correspAuthorsNote=, copyrightStatement=null, copyrightOwner=null, extLink=null, articleAbsUrl=null, sourceXml=y/cBVdFa04CSLU8vRiyZIA==, magXml=3RuxunW5hhENPMQGcmBQRg==, pdfUrl=null, pdf=null, pdfFileSize=null, pdfExtLink=null, richHtmlUrl=null, mobilePdfUrl=null, reviewReport=null, pdfFirstPage=null, abstractGraph=bI+fgYKirUeaonwgKJm2TQ==, abstractGraphContent=null, abstractVideo=null, citation=null, cebUrl=null, magXmlContent=fN/oH9FPt5cAREykUr9SGA==, mapNumber=null, fund=null)}, authors=[Author(id=1322941683675050097, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322941676129497169, orderNo=0, firstName=null, middleName=null, lastName=null, nameCn=null, orcid=null, stid=null, country=null, authorPic=null, dead=0, email=zhangxing990115@163.com, emailSecond=null, emailThird=null, correspondingAuthor=0, authorType=1, ext={EN=AuthorExt(id=1322941684132229235, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322941676129497169, authorId=1322941683675050097, language=EN, stringName=XING ZHANG, firstName=XING, middleName=null, lastName=ZHANG, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=1, address=¹ School of Energy Resources, China University of Geosciences (Beijing), Beijing 100083, China, bio=null, bioImg=null, bioContent=null, aboutCorrespAuthor=null), CN=AuthorExt(id=1322941684203532404, tenantId=1146029695717560320, journalId=1322258508890079423, articleId=1322941676129497169, authorId=1322941683675050097, language=CN, stringName=张星, firstName=null, middleName=null, lastName=null, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=1, address=¹　中国地质大学（北京）能源学院，北京　 　100083, bio={"content":"

张星（1999—），男，在读博士研究生，主要从事非常规储层天然裂缝形成机理及表征预测、储层质量评价方面的研究。地址：北京市海淀区学院路29号，邮政编码：100083。E-mail：zhangxing990115@163.com

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张星（1999—），男，在读博士研究生，主要从事非常规储层天然裂缝形成机理及表征预测、储层质量评价方面的研究。地址：北京市海淀区学院路29号，邮政编码：100083。E-mail：zhangxing990115@163.com

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