歧口凹陷热液流体活动及其对储集层的改造

侯中帅; 周立宏; 金凤鸣; 陈世悦; 蒲秀刚; 鄢继华; 李宏军

doi:10.3799/dqkx.2019.282

Volume 46 Issue 1

Jan. 2021

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Article Navigation > Earth Science > 2021 > 46(1): 200-214

Hou Zhongshuai, Zhou Lihong, Jin Fengming, Chen Shiyue, Pu Xiugang, Yan Jihua, Li Hongjun, 2021. Hydrothermal Fluid Activity and Its Reformation on Reservoirs in Qikou Depression. Earth Science, 46(1): 200-214. doi: 10.3799/dqkx.2019.282

Citation:

Hou Zhongshuai, Zhou Lihong, Jin Fengming, Chen Shiyue, Pu Xiugang, Yan Jihua, Li Hongjun, 2021. Hydrothermal Fluid Activity and Its Reformation on Reservoirs in Qikou Depression. Earth Science, 46(1): 200-214. doi: 10.3799/dqkx.2019.282

Citation:

Hou Zhongshuai, Zhou Lihong, Jin Fengming, Chen Shiyue, Pu Xiugang, Yan Jihua, Li Hongjun, 2021. Hydrothermal Fluid Activity and Its Reformation on Reservoirs in Qikou Depression. Earth Science, 46(1): 200-214. doi: 10.3799/dqkx.2019.282

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Hydrothermal Fluid Activity and Its Reformation on Reservoirs in Qikou Depression

doi: 10.3799/dqkx.2019.282

1.
Interdisciplinary Science Research Institute, Hebei GEO University, Shijiazhuang 050031, China
2.
School of Geocinseces, China University of Petroleum, Qingdao 266580, China
3.
Petrochina Dagang Oilfield Compamy, Tianjin 300280, China

Received Date: 2019-11-23
Publish Date: 2021-01-15

Abstract

Abstract

In order to clarify the development characteristics of the hydrothermal fluid activity and its reformation effect on the reservoir in the oil-rich depression, the Qikou depression in the Bohai Bay basin was studied. Based on the analysis of core, thin sections, XRF, SEM, salinity of formation water, pyrolysis, homogenization temperature of inclusions, clay minerals, trace elements, REE and conventional physical properties, the evidences of hydrothermal fluid activity in Qikou depression of Bohai Bay basin were analyzed, and the reformation patterns on different types of reservoirs were identified. we regard that the hydrothermal fluid activity in the Qikou depression is relatively developed and has a strong reformation effect on the reservoir. The results show that there are several types of hydrothermal fluid activity indicators in the Qikou depression, including:hydrothermal breccia, zebra fabric, faded mudstone and several kinds of hydrothermal mineral associations; abnormally high formation water salinity; mudstones with abnormally high T_max or S₁ and S₂ values; the homogenization temperature of inclusion exceeding the maximum temperature of normal thermal evolution; the abnormally high content of kaolinite in shallow strata sandstones and the abnormally high content of chlorite in mid-deep strata sandstones; the abnormally high characteristics of trace elements such as Zn、Cd、Ba and Pb in mudstones; the rare earth elements in carbonate rocks showing Eu positive anomaly. In different kinds of reservoirs, the reformation patterns of hydrothermal fluid are different:hydraulic fracturing and dissolution are mainly developed in the carbonate rocks, hydraulic fracturing and promoting devitrification are mainly developed in the tuff, hydraulic fracturing is mainly developed in the basalt, while the hydrothermal fluid reform sandstone reservoirs by dissolution and promoting chlorite development.
- hydrothermal fluid,
- reservoir reformation,
- Qikou depression,
- reformation pattern,
- petroleum geology

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References(52)

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Hydrothermal Fluid Activity and Its Reformation on Reservoirs in Qikou Depression

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