莱州湾凹陷火山岩-湖相碳酸盐岩混积岩储层特征和成因

刘晓健; 王清斌; 代黎明; 刘士磊; 郝轶伟

doi:10.3799/dqkx.2020.119

Volume 45 Issue 10

Nov. 2020

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Article Navigation > Earth Science > 2020 > 45(10): 3579-3588

Liu Xiaojian, Wang Qingbin, Dai Liming, Liu Shilei, Hao Yiwei, 2020. Reservoir Characteristics and Formation Mechanisms of Lacustrine Carbonate and Volcanics Mixing Sediments, Laizhouwan Sag. Earth Science, 45(10): 3579-3588. doi: 10.3799/dqkx.2020.119

Citation:

Liu Xiaojian, Wang Qingbin, Dai Liming, Liu Shilei, Hao Yiwei, 2020. Reservoir Characteristics and Formation Mechanisms of Lacustrine Carbonate and Volcanics Mixing Sediments, Laizhouwan Sag. Earth Science, 45(10): 3579-3588. doi: 10.3799/dqkx.2020.119

Citation:

Liu Xiaojian, Wang Qingbin, Dai Liming, Liu Shilei, Hao Yiwei, 2020. Reservoir Characteristics and Formation Mechanisms of Lacustrine Carbonate and Volcanics Mixing Sediments, Laizhouwan Sag. Earth Science, 45(10): 3579-3588. doi: 10.3799/dqkx.2020.119

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Reservoir Characteristics and Formation Mechanisms of Lacustrine Carbonate and Volcanics Mixing Sediments, Laizhouwan Sag

doi: 10.3799/dqkx.2020.119

Tianjin Branch of China National Offshore Oil Corporation Limited, Tianjin 300459, China

Received Date: 2020-03-06
Publish Date: 2020-11-17

Abstract

Abstract

It is the first time to find the mixed deposition of lacustrine carbonate and volcanics in Shahejie Formation, Laizhouwan sag, Bohai Sea area. The genetic mechanism of this kind of reservoir is not clear. By casting thin section, Ar-ion milling scanning electron microscope and core 3D CT scanning data, it is confirmed that the interstitial rock is a double medium storage space of pores and fractures. The lacustrine carbonate sediments were accompanied by intermittent eruptions of volcanic activities during the sedimentary period, and four kinds of mixed sedimentary modes developed. Volcanic eruptions provide a large number of tuff components which provide conditions for fluid selective dissolution. In addition, the fossils of microcodium were found in the strata, indicating that the interstitial rocks had undergone long-term exposure, and the interstitial rocks had undergone atmospheric water weathering and leaching. A large number of vertical fractures and horizontal slippage joints between low angle layers were formed in the reservoir due to tectonic action. The superposition of fractures and dissolution pores forms a fracture-pore reservoir.
- mixd sediment,
- volcanic rock,
- lacustrine carbonate rock,
- reservoir genesis,
- Laizhouwan sag,
- sedimentation

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References(45)

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