Geochemistry of pore water and associated diagenetic reactions in the diapiric area of Yinggehai Basin, northwestern South China Sea

Tao Jiang; Xinong Xie; Hui Chen; Zhenfeng Wang; Xushen Li

doi:10.1007/s12583-015-0526-y

Volume 26 Issue 3

Jul 2015

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Journal of Earth Science > 2015 > 26(3): 306-316.

Tao Jiang, Xinong Xie, Hui Chen, Zhenfeng Wang, Xushen Li. Geochemistry of pore water and associated diagenetic reactions in the diapiric area of Yinggehai Basin, northwestern South China Sea. Journal of Earth Science, 2015, 26(3): 306-316. doi: 10.1007/s12583-015-0526-y

Citation:

Tao Jiang, Xinong Xie, Hui Chen, Zhenfeng Wang, Xushen Li. Geochemistry of pore water and associated diagenetic reactions in the diapiric area of Yinggehai Basin, northwestern South China Sea. Journal of Earth Science, 2015, 26(3): 306-316. doi: 10.1007/s12583-015-0526-y

Citation:

Tao Jiang, Xinong Xie, Hui Chen, Zhenfeng Wang, Xushen Li. Geochemistry of pore water and associated diagenetic reactions in the diapiric area of Yinggehai Basin, northwestern South China Sea. Journal of Earth Science, 2015, 26(3): 306-316. doi: 10.1007/s12583-015-0526-y

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Geochemistry of pore water and associated diagenetic reactions in the diapiric area of Yinggehai Basin, northwestern South China Sea

doi: 10.1007/s12583-015-0526-y

1.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, China
2.
Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology, Kochi 783-8502, Japan
3.
China National Offshore Oil Zhanjiang Ltd. Corporation, Zhanjiang 524057, China

More Information

Corresponding author: Tao Jiang, taojiang@cug.edu.cn
Received Date: 18 Oct 2014
Accepted Date: 15 Feb 2015
Publish Date: 01 Jun 2015

Abstract

Abstract

This study examined the geochemical features of pore water in the diapiric area of the Yinggehai Basin, northwestern South China Sea, and illuminated the origin and evolution of basin fluids. Pore water with low salinity occurs in marine sediments in the diapiric area even without meteoric water infiltration. The presence of low-salinity water within deep, overpressured compartments is assumed to be due to smectite-illite transformation. Howerver, in shallow portions (less than 2 000 m) of diapiric areas with normal pressure, pore water has a much wider variation and much lower salinity than that in the overpressured intervals. Its total dissolved solid (TDS) content is ~5 336 to 35 939 mg/L. Moreover, smectite and chlorite content sharply decreases as kaolinite and illite content increase in shallower intervals. The geochemical variation of pore water in diapiric structures indicates the expulsion of low-salinity, overpressured fluids along vertical faults. Strong injection of hot fluids from deep overpressured sediments results in rapid clay mineral transformation in shallow reservoirs. Consequently, fluid mixing due to fluid expulsion from deeper overpressured deposits leads to variation in salinity and ionic composition as well as some diagenetic reactions. This includes transformation of clay minerals caused by the higher temperatur of deeper hot fluids, e.g., the transfromation of smectite to illite and chlorite to kaolinite. Therefore, variations in salinity and ionic compositions in various pressured systems provide a clue to flow pathways and associated diagenetic reactions.
- pore water,
- diagenetic reaction,
- clay mineral transformation,
- overpressured system,
- Yinggehai Basin

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Geochemistry of pore water and associated diagenetic reactions in the diapiric area of Yinggehai Basin, northwestern South China Sea

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Geochemistry of pore water and associated diagenetic reactions in the diapiric area of Yinggehai Basin, northwestern South China Sea

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