Effect of sedimentary environment on shale lithofacies in the lower third member of the Shahejie Formation, Zhanhua Sag, eastern China
Li, Tingwei1,2; Jiang, Zhenxue1,2; Xu, Chenlu3; Yuan, Yuan3; Wang, Pengfei1,2; Liu, Guoheng1; Zhang, Bo1,2; Ning, Chuanxiang1,2; Wang, Zhi1,2
刊名INTERPRETATION-A JOURNAL OF SUBSURFACE CHARACTERIZATION
2017-11-01
卷号5期号:4页码:T487-T501
ISSN号2324-8858
DOI10.1190/INT-2017-0016.1
文献子类Article
英文摘要Research on shale lithofacies is important for shale oil and gas production. This study focused on the lower third member of the Shahejie Formation (Es-3(l)) in the Luo-69 well in the Zhanhua Sag, Jiyang Depression, Bohai Bay Basin, eastern China. Several methods, including thin section observations, total organic carbon (TOC) analysis, X-ray diffraction analysis, quantitative evaluations of minerals by scanning electron microscopy, major and trace-element analyses, and field emission-scanning electron microscopy, are used to investigate the effect of sedimentary environment on the type and distribution of shale lithofacies. Our research indicates that 36 types of shale lithofacies can be classified based on the TOC content, mineral composition, and sedimentary structure, of which five types are identified in the study area. The Es-3(l) shale has a high calcareousmineral content (average of 49.64%), low clay and siliceous minerals contents (averages of 19.54% and 19.02%, respectively), a high TOC content (average of 3.00 wt%), and well-developed horizontal bedding. The sedimentary environment during the deposition of the Es-3(l) shale in the Zhanhua Sag had a warm and moist climate, limited provenance, saline water, and strong reducibility. The sedimentary environment in the early stage had a drier climate, more limited provenance, higher salinity, and stronger reducibility than that in the later stage. Shale lithofacies can reflect a certain sedimentary environment and depositional process; similarly, a depositional environment controls the type and distribution of shale lithofacies. Due to the characteristics of the Es-3(l) sedimentary environment, organic-rich massive mixed shale, organic-rich bedded mixed-calcareous shale, organic-rich laminated calcareous shale, and organic-fair laminated calcareous shale are developed in the Es-3(l) formation from top to bottom.
WOS关键词MISSISSIPPIAN BARNETT SHALE ; FORT-WORTH BASIN ; OCEANIC ANOXIC EVENT ; NORTH-CENTRAL TEXAS ; REDOX CONDITIONS ; TRACE-ELEMENTS ; SICHUAN BASIN ; GAS SYSTEMS ; GEOCHEMISTRY ; PORES
WOS研究方向Geochemistry & Geophysics
语种英语
出版者SOC EXPLORATION GEOPHYSICISTS
WOS记录号WOS:000412938100017
资助机构National Basic Research Program of China (973 Project)(2014CB239105) ; National Basic Research Program of China (973 Project)(2014CB239105) ; National Basic Research Program of China (973 Project)(2014CB239105) ; National Basic Research Program of China (973 Project)(2014CB239105)
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/61985]  
专题地质与地球物理研究所_中国科学院油气资源研究重点实验室
通讯作者Li, Tingwei
作者单位1.China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing, Peoples R China
2.China Univ Petr, Unconvent Nat Gas Res Inst, Beijing, Peoples R China
3.Chinese Acad Sci, Key Lab Petr Resource Res, Inst Geol & Geophys, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Li, Tingwei,Jiang, Zhenxue,Xu, Chenlu,et al. Effect of sedimentary environment on shale lithofacies in the lower third member of the Shahejie Formation, Zhanhua Sag, eastern China[J]. INTERPRETATION-A JOURNAL OF SUBSURFACE CHARACTERIZATION,2017,5(4):T487-T501.
APA Li, Tingwei.,Jiang, Zhenxue.,Xu, Chenlu.,Yuan, Yuan.,Wang, Pengfei.,...&Wang, Zhi.(2017).Effect of sedimentary environment on shale lithofacies in the lower third member of the Shahejie Formation, Zhanhua Sag, eastern China.INTERPRETATION-A JOURNAL OF SUBSURFACE CHARACTERIZATION,5(4),T487-T501.
MLA Li, Tingwei,et al."Effect of sedimentary environment on shale lithofacies in the lower third member of the Shahejie Formation, Zhanhua Sag, eastern China".INTERPRETATION-A JOURNAL OF SUBSURFACE CHARACTERIZATION 5.4(2017):T487-T501.
个性服务
查看访问统计
相关权益政策
暂无数据
收藏/分享
所有评论 (0)
暂无评论
 

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。


©版权所有 ©2017 CSpace - Powered by CSpace