鄂尔多斯盆地南部延长组长7段富有机质泥页岩生烃条件及沉积模式分析  

HYDROCARBON GENERATION CONDITIONS AND SEDIMENTARY MODEL OF ORGANIC-RICH SHALE FROM CHANG 7 MEMBER OF YANCHANG FROMATION IN SOUTHERN ORDOS BASIN

作　　者：师学耀[1] 高超利 雷俊杰[1] 黄闯 安鑫胜 张宇恒 王如意 李艳青 王磊[1] 孙宁亮 SHI Xue-yao;GAO Chao-li;LEI Jun-jie;HUANG Chuang;AN Xin-sheng;ZHANG Yu-heng;WANG Ru-yi;LI Yan-qing;WANG Lei;SUN Ning-liang(Research Center for Exploration and Development Technology,Yanchang Oilfield Co.,Ltd.,Yan’an 716000,Shaanxi Province,China;School of Petroleum Engineering,China University of Petroleum,Beijing 102249,China;School of Resources and Civil Engineering,Northeastern University,Shenyang 110819,China)

机构地区：[1]延长油田股份有限公司勘探开发技术研究中心,陕西延安716000 [2]中国石油大学石油工程学院,北京102249 [3]东北大学资源与土木工程学院,辽宁沈阳110819

出　　处：《地质与资源》2023年第1期39-48,69,共11页Geology and Resources

基　　金：国家科技重大专项项目“大型油气田及煤层气开发-砂页岩储层特征及有利区带评价”(2016ZX05066001-003);延长油田股份有限公司科技项目基金“志丹油田爬子洼区石油地质评价及勘探建议”(ycsh2021ky-B-15-1-3)。

摘　　要：针对鄂尔多斯盆地南部延长组长7段富有机质泥页岩岩石学特征及生烃潜力认识不清的问题,通过对研究区泥页岩的岩石学、矿物组成、有机地球化学、孔隙类型及沉积模式精细研究,结果表明:研究区主要存在3种不同类型的泥页岩,分别是泥质碎屑流成因的块状泥岩、浊流成因的正粒序泥岩及沉积于静水环境中的纹层状泥岩.块状泥岩和正粒序泥岩含有较多的陆源碎屑矿物,纹层状泥岩碳酸盐矿物含量高,同时含有较高的有机碳及可溶烃和热解烃,它们的干酪根类型以Ⅱ型为主,含有少量Ⅰ型.泥页岩储集空间主要为粒间孔、粒内孔及微裂缝,有机质孔少见,纹层状泥岩孔隙类型多样,储集空间大.泥质碎屑流形成的块状泥岩沉积在湖盆坡脚处,浊流成因的正粒序泥岩及纹层状泥岩广泛沉积于湖盆中心,且厚度大.The study on petrology,mineral composition,organic geochemistry,pore types and sedimentary model of shale from Chang 7 Member of Yanchang Formation in southern Ordos Basin shows that there are three types of mud shale in the area,including massive mudstone of muddy debris flow origin,normal-graded mudstone formed by turbidity current,and laminated mudstone deposited in lentic environment.The former two contain numerous terrigenous clastic minerals,while the latter has high content of carbonate minerals as well as high organic carbon and soluble and pyrolysed hydrocarbon.The kerogens of the mud shale are dominated by type II with minus of type I.The reservoir space of shale is mainly intergranular pore,intragranular pore and microfracture,with rare organic pore.The laminated mudstones are characterized by various pore types and large reservoir space.The massive mudstones formed by muddy debris flow are deposited at the slope toe of lake basin,while the normal-graded mudstone of turbidity current origin and laminated mudstone are widely deposited in the center of lake basin with large thickness.

关 键 词：富有机质泥岩 页岩油气 生烃条件 地球化学特征 沉积模式 鄂尔多斯盆地 

分 类 号：P618.13[天文地球—矿床学]