中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Diagenesis of microbialite-dominated carbonates in the Upper Ediacaran Qigebrak Formation, NW Tarim Basin, China: Implications for reservoir development

文献类型:期刊论文

作者Tang, Pan1,2,3; Chen, Daizhao1,2,3; Wang, Yuanzheng1,2,3; Ding, Yi4; El-Shafeiy, Moataz1,5; Yang, Bo1,2,3
刊名MARINE AND PETROLEUM GEOLOGY
出版日期2022-02-01
卷号136页码:15
关键词Diagenesis Microbialites Pore systems Upper Ediacaran Reservoir development
ISSN号0264-8172
DOI10.1016/j.marpetgeo.2021.105476
英文摘要The interests in deeply-buried hydrocarbon reservoirs increase rapidly with increasing performances into greater depths. The ancient Ediacaran Qigebrak Formation microbialites in Tarim Basin are widespread and increasingly considered as a potential hydrocarbon exploration target for deeply-buried carbonate reservoirs. However, controlling factors on the development of microbialite reservoirs have not well been understood yet. This work was conducted upon microbialites of the Qigebrak Formation, Aksu, NW Tarim Basin based on detailed petrological, geochemical, and petrophysical investigations, aiming at understanding the diagenetic processes and influences on the porosity generation and preservation. The investigated dolomicrobialites, encompass four distinctive lithofacies types: microbial laminite, stromatolite, spongiomicrobialite, and microbial-peloidal wackstone/packstone. The main diagenetic minerals consist of three types of dolomite (microbial dolomicrite, early-stage fibrous dolomite cement, and late-stage pore filling dolomite cement), quartz, calcite and bitumen fillings. Pore spaces are dominated by vugs, solution-enhanced pores, microbial framework pores, intercrystalline pores, micropores and fractures. Among all the microbialites, spongiomicrobialites have porosity averaging 6.15% and permeability averaging 0.20 mD, which show better petrophysical properties than other microbialites. This study pinpoints that the development of a high quality microbialite reservoir in the studied area was essentially controlled by three controlling factors: microbial mat deposition, early dolomitization, and meteoric karst leaching. Microbial mat deposits can be considered as the foundation to form framework pores. Furthermore, the early dolomitization increased the resistivity of the studied microbialites toward chemical and physical compaction, during which abundant micropores are generated. The meteoric karst dissolution, which is related to the uppermost Qigebrak Formation unconformity surface, is the crucial controlling factor that enhanced the porosity via forming a large quantity of vugs- and solution-related pores. This study attempts to better understand the microbialites diagenesis that may have affected the reservoir property, and to serve as an analog for the similar microbialite reservoirs in other areas of China.
WOS关键词TRIASSIC LEIKOUPO FORMATION ; FORMATION MECHANISM ; LOWER ORDOVICIAN ; SICHUAN BASIN ; EVOLUTION ; DOLOMITE ; POROSITY ; AREA ; GEOCHEMISTRY ; ENVIRONMENT
资助项目National Key Research and Development (R & D) Program of China[2017YFC0603103] ; National Natural Science Foundation of China[U19B6003]
WOS研究方向Geology
语种英语
WOS记录号WOS:000748860100002
出版者ELSEVIER SCI LTD
资助机构National Key Research and Development (R & D) Program of China ; National Key Research and Development (R & D) Program of China ; National Key Research and Development (R & D) Program of China ; National Key Research and Development (R & D) Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development (R & D) Program of China ; National Key Research and Development (R & D) Program of China ; National Key Research and Development (R & D) Program of China ; National Key Research and Development (R & D) Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development (R & D) Program of China ; National Key Research and Development (R & D) Program of China ; National Key Research and Development (R & D) Program of China ; National Key Research and Development (R & D) Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development (R & D) Program of China ; National Key Research and Development (R & D) Program of China ; National Key Research and Development (R & D) Program of China ; National Key Research and Development (R & D) Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/104012]  
专题地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
通讯作者Chen, Daizhao
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
4.Chengdu Univ Technol, State Key Lab Oil & Gas Reservoir Geol & Exploita, Chengdu 610059, Peoples R China
5.Cairo Univ, Fac Sci, Geol Dept, Giza, Egypt
推荐引用方式
GB/T 7714
Tang, Pan,Chen, Daizhao,Wang, Yuanzheng,et al. Diagenesis of microbialite-dominated carbonates in the Upper Ediacaran Qigebrak Formation, NW Tarim Basin, China: Implications for reservoir development[J]. MARINE AND PETROLEUM GEOLOGY,2022,136:15.
APA Tang, Pan,Chen, Daizhao,Wang, Yuanzheng,Ding, Yi,El-Shafeiy, Moataz,&Yang, Bo.(2022).Diagenesis of microbialite-dominated carbonates in the Upper Ediacaran Qigebrak Formation, NW Tarim Basin, China: Implications for reservoir development.MARINE AND PETROLEUM GEOLOGY,136,15.
MLA Tang, Pan,et al."Diagenesis of microbialite-dominated carbonates in the Upper Ediacaran Qigebrak Formation, NW Tarim Basin, China: Implications for reservoir development".MARINE AND PETROLEUM GEOLOGY 136(2022):15.

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来源:地质与地球物理研究所

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