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ID:36771931
大小:1.59 MB
页数:6页
时间:2019-05-15
《塔北草湖凹陷形成演化新认识及油气地质意义》由会员上传分享,免费在线阅读,更多相关内容在行业资料-天天文库。
1、学兔兔www.xuetutu.com专天然气比第34卷第3期OIL&GASGE0LOGY2013年6月文章编号:0253—9985(2013)03—0370—06doi:10.11743/ogg20130313塔北草湖凹陷形成演化新及油气地质意义姚泽伟,何光玉,郑晓丽,漆立新2,张洪安,云露,林璐,王文侠(1.浙江大学地球科学系,浙江杭州,310027;2.中国石化西北油田分公司,新疆乌鲁木齐,830011)摘要:基于二维地震剖面的精细地质解释,并结合钻井资料的分析,提出了塔北地区古生代以来草湖凹陷形成演化的新认识,认为塔北草湖凹陷东、西两侧斜坡的形成时间与形成机理存在明显的
2、差异。凹陷西侧中一上奥陶统自东向西超覆沉积特征明显,表明西斜坡主要形成于加里东中期,形成机理是在持续区域挤压背景下,草湖地区相对沉降,阿克库勒地区相对隆升,表现出沉积型凹陷斜坡的特征;而凹陷东侧可见奥陶系、志留系等地层被强烈抬升并遭受剥蚀,角度不整合于上泥盆统一石炭系之下,后者又角度不整合于三叠系之下,表明东斜坡主要形成于加里东晚期和海西早、晚期的强烈构造变形,以海西晚期为主,表现出构造型凹陷斜坡的特征。草湖凹陷西侧有利于发育下奥陶统岩溶型地层圈闭,凹陷东侧有利于发育志留系、石炭系和三叠系超覆型岩性圈闭及中一上奥陶统不整合型地层圈闭、下奥陶统岩溶型地层圈闭,它们是下一步油气勘
3、探的重要方向。关键词:沉积型凹陷斜坡;构造型凹陷斜坡;油气圈闭;古生代;草湖凹陷;塔里木盆地中图分类号:TEl21.1文献标识码:ANewideasabouttheevolutionofCaohusaginthenorthernTarimBasinanditssignificanceforpetroleumgeologyYaoZewei,HeGuangyu,ZhengXiaoli,QiLixin,ZhangHong’an,YunLu,LinLu,WangWenxia(1.DepartmentofEaahSciences,ZhejiangUniversity,Hangzhou,
4、Zhejiang310027,China;2.NorthwestOilfieldCompanyofSINOPEC,Urumqi,Xinjiang830011,China)Abstract:TheevolutionofCaohusaginno~hernTarimBasinisdiscussedinthispaperbasedongeologicalinterpretationoftwo-dimensionalseismicprofilesandanalysisofdrillingdata.WepresentnewideasabouttheevolutionofCaohusags
5、incePaleozoic.ThetimeandmechanismofformationoftheeasternandwesternslopesofCaohusagareapparentlydif-ferent.Inthewesternsideofthesag,theMiddle—UpperOrdovicianshowdistinctoverlappingcharacteristicsfromeasttowest,indicatingthatthewesternslopeofCaohusagwasdevelopedmainlyintheMiddleCaledonianasth
6、eresultofthesubsidingofCaohuareaandtheupliftingofAkekuleUpliftunderthecontinuousregionalcompression.Thewesternslopehasthecharacteristicsofdepositionalsagslope.Whileintheeasternsideofthesag,theSilurian—OrdovicianwerestronglyupliftedanderodedandunderlieunconformablytheUpperDevonian-Carbonifer
7、ous,whichinturnunderlieunconformablytheTriassic.ThisdemonstratesthattheeasternslopewasdevelopedintheLateCaledonianaswellastheEarlyandLateHercynianastheresultoftheintensetectonicdeformation,withtheLateHercynianbeingthedominant.Theeast-ernslopeshowsthechar
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