Space-Time Evolution and Controlling Factor of Fine-Grained Sediments in the Upper Fourth Member of Shahejie Formation, Dongying Depression

Guoqi Song; Jing Wu; Yong Wang; Xuefeng Hao

doi:10.1007/s12583-016-0938-3

Volume 28 Issue 6

Nov 2017

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Journal of Earth Science > 2017 > 28(6): 987-995.

Guoqi Song, Jing Wu, Yong Wang, Xuefeng Hao. Space-Time Evolution and Controlling Factor of Fine-Grained Sediments in the Upper Fourth Member of Shahejie Formation, Dongying Depression. Journal of Earth Science, 2017, 28(6): 987-995. doi: 10.1007/s12583-016-0938-3

Citation:

Guoqi Song, Jing Wu, Yong Wang, Xuefeng Hao. Space-Time Evolution and Controlling Factor of Fine-Grained Sediments in the Upper Fourth Member of Shahejie Formation, Dongying Depression. Journal of Earth Science, 2017, 28(6): 987-995. doi: 10.1007/s12583-016-0938-3

Citation:

Guoqi Song, Jing Wu, Yong Wang, Xuefeng Hao. Space-Time Evolution and Controlling Factor of Fine-Grained Sediments in the Upper Fourth Member of Shahejie Formation, Dongying Depression. Journal of Earth Science, 2017, 28(6): 987-995. doi: 10.1007/s12583-016-0938-3

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Space-Time Evolution and Controlling Factor of Fine-Grained Sediments in the Upper Fourth Member of Shahejie Formation, Dongying Depression

doi: 10.1007/s12583-016-0938-3

Guoqi Song¹,
Jing Wu^{2,3
,
,},
Yong Wang¹,
Xuefeng Hao¹

1.
Geological Science Research Institute, SINOPEC Shengli Oilfield Company, Dongying 257000, China
2.
Petroleum Exploration and Production Research Institute of SINOPEC, Beijing 100083, China
3.
SINOPEC Key Laboratory of Shale Gas/Oil Exploration & Production, Beijing 100083, China

More Information

Corresponding author: Jing Wu, wujing6524982@163.com
Received Date: 11 May 2016
Accepted Date: 30 Nov 2016
Publish Date: 01 Dec 2017

Abstract

Abstract

Fine-grained rocks (FGR) are the important source rocks and reservoirs of shale hydrocarbon which is the prospect hotspot at present. Widely distributed fine-grained sediments (FGS) of the upper fourth member of Shahejie Formation in Dongying depression are taken as an example to study the space-time evolution and controlling factor of FGS in this paper. Based on the analysis of well cores, thin sections, inorganic and organic geochemistry indicators, FGR are divided into 7 types of lithofacies. Through the study of 'point-line-plane', this study shows that FGS has the characteristics of rhythum, diversity and succession. The first stage is characterized by clayey FGS (massive claystone). The second stage is characterized by carbonate FGS (low-TOC laminated limestone) and dolomitic FGS (dolomitic-silty shale) formed by transgression. The third stage is characterized by organic-rich carbonate FGS (middle/high-TOC laminated limestone) distributed in cycle. The fourth stage is characterized by FGS mixed carbonate and siliciclastic sediments (calcareous-silty shale). A variety of space-time evolution of FGS are controlled by multiple factors including tectonism, climate and lake conditions.
- fine-grained sediments,
- lithofacies,
- space-time evolution,
- controlling factor,
- Dongying depression,
- the upper fourth member of Shahejie Formation

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References(37)

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