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鄂尔多斯盆地合水地区长7致密油岩性岩相类型识别及其应用
引用本文:冉冶,王贵文,周正龙,赖锦,代全齐,陈晶,范旭强,王抒忱. 鄂尔多斯盆地合水地区长7致密油岩性岩相类型识别及其应用[J]. 中国地质, 2016, 0(4): 1331-1340
作者姓名:冉冶  王贵文  周正龙  赖锦  代全齐  陈晶  范旭强  王抒忱
作者单位:中国石油大学(北京)地球科学学院, 北京 102249,中国石油大学(北京)地球科学学院, 北京 102249;中国石油大学(北京)油气资源与探测国家重点实验室, 北京 102249,中国石油大学(北京)地球科学学院, 北京 102249,中国石油大学(北京)地球科学学院, 北京 102249,中国石油大学(北京)非常规天然气研究院, 北京 102249,中国石油大学(北京)地球科学学院, 北京 102249,中国石油大学(北京)地球科学学院, 北京 102249,中国石油大学(北京)地球科学学院, 北京 102249
基金项目:国家十二五科技重大专项(2011ZX05020-008)和国家自然科学基金(41472115)联合资助。
摘    要:利用岩心、薄片、常规测井、成像测井等资料结合物性分析等,对鄂尔多斯盆地合水地区长7致密油岩性岩相等特征进行了研究。长7致密油储层以砂质碎屑流、浊流和滑塌成因的砂岩为主,烃源岩以泥岩、油页岩为主,根据粒度参数进一步将长7致密油岩性岩相划分为砂质碎屑流细砂岩相、浊流细砂岩相、浊流粉砂岩相、滑塌岩相、半深湖—深湖泥岩相以及油页岩相6类。通过岩心刻度常规和成像测井,建立了不同岩性岩相的测井识别评价标准,并实现了各单井纵向上的岩性岩相的识别和划分。在此基础上,进一步探讨了不同岩性岩相与TOC含量和脆性指数的关系。最后结合试油气资料和油气解释结论,阐明岩性岩相对致密油储层物性和含油气性的定量控制。致密油岩性岩相的研究可为后期成岩相、孔隙结构以及优质储集体预测等奠定基础,为研究区长7致密油的综合评价和有利发育区带预测提供理论指导和技术支持。

关 键 词:岩性岩相  致密油  TOC  脆性指数  长7段  合水地区  鄂尔多斯盆地
收稿时间:2015-07-12
修稿时间:2015-10-25

Identification of lithology and lithofacies type and its application to Chang 7 tight oil in Heshui area, Ordos Basin
RAN Ye,WANG Gui-wen,ZHOU Zheng-long,LAI Jin,DAI Quan-qi,CHEN Jing,FAN Xu-qiang and WANG Shu-chen. Identification of lithology and lithofacies type and its application to Chang 7 tight oil in Heshui area, Ordos Basin[J]. Geology in China, 2016, 0(4): 1331-1340
Authors:RAN Ye  WANG Gui-wen  ZHOU Zheng-long  LAI Jin  DAI Quan-qi  CHEN Jing  FAN Xu-qiang  WANG Shu-chen
Affiliation:College of Geosciences, China University of Petroleum, Beijing 102249, China,College of Geosciences, China University of Petroleum, Beijing 102249, China;State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing 102249, China,College of Geosciences, China University of Petroleum, Beijing 102249, China,College of Geosciences, China University of Petroleum, Beijing 102249, China,Unconventional Natural Gas Institute, China University of Petroleum, Beijing 102249, China,College of Geosciences, China University of Petroleum, Beijing 102249, China,College of Geosciences, China University of Petroleum, Beijing 102249, China and College of Geosciences, China University of Petroleum, Beijing 102249, China
Abstract:The characteristics of lithology and lithofacies in Chang 7 tight oil in Heshui area, Ordos Basin, were studied by such means as core observation, traditional thin section analysis, conventional logging and imaging logging processing, combined with general physical analysis. Chang 7 tight oil reservoir is mainly sandstone caused jointly by sandy debris flow, turbidity current and slump, and source rocks are mainly mudstone and oil shale. According to grain size parameters, Chang 7 tight oil is further divided into six kinds of lithology and lithofacies, i.e., fine sandstone of sandy debris flow, fine sandstone of turbidity current, siltstone of turbidity current, fluxoturbidite, mudstone of semi-deep water or deep water and oil shale. According to conventional logging and imaging logging scaled by core data, the authors established the evaluation criteria of well logging identification in different kinds of lithology and lithofacies, realized the identification and classification of lithology and lithofacies in a single well on the longitude, and further explored the relationship between different kinds of lithology and lithofacies and TOC content as well as brittleness index. Finally oil-gas testing data and oil-gas interpretation results were combined to illuminate the quantitative control of lithology and lithofacies on physical property and oil-gas possibility of tight oil reservoir. The study of lithology and lithofacies of tight oil can lay the foundation for the further analysis of lithogenous phase and pore structure as well as the prediction of high quality reservoir. It can also provide theoretical guidance and technical support for the comprehensive assessment of Chang 7 tight oil and the prediction of favorable zones for oil-gas reservoir development.
Keywords:lithology and lithofacies  tight oil  TOC  brittleness index  Chang 7  Heshui area  Ordos Basin
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