中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Genetic mechanism of Cambrian dolostone in Bachu-Tazhong area, Tarim Basin, western China

文献类型:期刊论文

作者Cheng, Li -Juan2,5; Li, Zhong5; Liu, Bo2; Li, Jia-Wei4; Zhou, Yuan-Quan5; Ostadhassan, Mehdi1,2; Li, Hong-Xia2; Yao, Lin-Ru3
刊名ORE GEOLOGY REVIEWS
出版日期2023-06-01
卷号157页码:16
ISSN号0169-1368
关键词Dolomitization Evaporite Diagenetic systems Tarim Basin
DOI10.1016/j.oregeorev.2023.105445
英文摘要Abundant energy resources that are found in Tarim Basin are hosted in pervasively dolomitized carbonates of the Cambrian age. The thick dolostone is distributed widely, deeply buried and quite complex in diagenesis. The middle Cambrian gypsum sequence is widespread in west of the Tarim basin. From bottom to top, the Cambrian is divided into pre-salt, inter-salt and post-salt with various diagenesis types and degree causing different sealing properties. Subsurface core samples from the three systems were studied using cathodoluminescence (CL), isotope studies (813C, 818O and 87Sr/86Sr), fluid inclusion, and elemental analysis for rare earth elements (TREE) to determine the origin of the dolomitizing fluids. Trace elements and isotope data show that high salinity seawater was most likely responsible for dolomitization of pre-salt system. Likewise, the pre-salt system has been the result of an open hydrothermal fluid transformation system. The inter-salt system was sealed by the upper gypsum layer and lower gypsum layer. The gypsum layer not only enhanced the sealing property of inter-salt strata but also impeded dolomitization, where the evaporating seawater caused dolomitization by refluxseepage process. Therefore, the inter-salt system was a nearly closed evaporation system dominated by the seawater. The geochemical parameters reveal that the post-salt system has a variety of fluid sources and mainly interacts with meteoric water and seawater, since the C isotope was clearly negative and Y/Ho ratio was found low(<30).
WOS关键词FREEZING-POINT DEPRESSION ; RARE-EARTH-ELEMENTS ; DOLOMITIZATION ; SEDIMENTARY ; RESERVOIRS ; GEOCHEMISTRY ; INCLUSIONS ; CARBONATES ; EVOLUTION ; HISTORY
资助项目Young Scholars in the North- east Petroleum University[2021YDL-21] ; National Natural Science Foundation of China[42002152] ; Research Foundation of Northeast Petroleum University
WOS研究方向Geology ; Mineralogy ; Mining & Mineral Processing
语种英语
出版者ELSEVIER
WOS记录号WOS:000988782600001
资助机构Young Scholars in the North- east Petroleum University ; Young Scholars in the North- east Petroleum University ; Young Scholars in the North- east Petroleum University ; Young Scholars in the North- east Petroleum University ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Research Foundation of Northeast Petroleum University ; Research Foundation of Northeast Petroleum University ; Research Foundation of Northeast Petroleum University ; Research Foundation of Northeast Petroleum University ; Young Scholars in the North- east Petroleum University ; Young Scholars in the North- east Petroleum University ; Young Scholars in the North- east Petroleum University ; Young Scholars in the North- east Petroleum University ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Research Foundation of Northeast Petroleum University ; Research Foundation of Northeast Petroleum University ; Research Foundation of Northeast Petroleum University ; Research Foundation of Northeast Petroleum University ; Young Scholars in the North- east Petroleum University ; Young Scholars in the North- east Petroleum University ; Young Scholars in the North- east Petroleum University ; Young Scholars in the North- east Petroleum University ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Research Foundation of Northeast Petroleum University ; Research Foundation of Northeast Petroleum University ; Research Foundation of Northeast Petroleum University ; Research Foundation of Northeast Petroleum University ; Young Scholars in the North- east Petroleum University ; Young Scholars in the North- east Petroleum University ; Young Scholars in the North- east Petroleum University ; Young Scholars in the North- east Petroleum University ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Research Foundation of Northeast Petroleum University ; Research Foundation of Northeast Petroleum University ; Research Foundation of Northeast Petroleum University ; Research Foundation of Northeast Petroleum University
源URL[http://ir.iggcas.ac.cn/handle/132A11/110906]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Cheng, Li -Juan
作者单位1.Univ Kiel, Inst Geosci Marine & Land Geomech & Geotecton, D-24118 Kiel, Germany
2.Northeast Petr Univ, Minist Educ, Key Lab Continental Shale Hydrocarbon Accumulat &, Daqing 163318, Peoples R China
3.Yushulin Oilfield Dev LLC, Inst Geol, Daqing 163000, Peoples R China
4.Res Inst Tsinghua Pearl River Delta, Guangzhou 510530, Peoples R China
5.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Cheng, Li -Juan,Li, Zhong,Liu, Bo,et al. Genetic mechanism of Cambrian dolostone in Bachu-Tazhong area, Tarim Basin, western China[J]. ORE GEOLOGY REVIEWS,2023,157:16.
APA Cheng, Li -Juan.,Li, Zhong.,Liu, Bo.,Li, Jia-Wei.,Zhou, Yuan-Quan.,...&Yao, Lin-Ru.(2023).Genetic mechanism of Cambrian dolostone in Bachu-Tazhong area, Tarim Basin, western China.ORE GEOLOGY REVIEWS,157,16.
MLA Cheng, Li -Juan,et al."Genetic mechanism of Cambrian dolostone in Bachu-Tazhong area, Tarim Basin, western China".ORE GEOLOGY REVIEWS 157(2023):16.

入库方式: OAI收割

来源:地质与地球物理研究所

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