玄武岩发育区砂岩储层特征及控制因素：渤海南部BZ34-9区与KL6区块对比

王维; 杨香华; 叶加仁; 王清斌; 朱红涛; 李欢

doi:10.3799/dqkx.2017.045

Volume 42 Issue 4

Apr. 2017

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Article Navigation > Earth Science > 2017 > 42(4): 570-586

Wang Wei, Yang Xianghua, Ye Jiaren, Wang Qingbin, Zhu Hongtao, Li Huan, 2017. Characterization and Controlling Factors of Sandstone Reservoirs in Basalt Development Areas: An Example from Comparison between BZ34-9 and KL6 Areas in South of Bohai Sea. Earth Science, 42(4): 570-586. doi: 10.3799/dqkx.2017.045

Citation:

Wang Wei, Yang Xianghua, Ye Jiaren, Wang Qingbin, Zhu Hongtao, Li Huan, 2017. Characterization and Controlling Factors of Sandstone Reservoirs in Basalt Development Areas: An Example from Comparison between BZ34-9 and KL6 Areas in South of Bohai Sea. Earth Science, 42(4): 570-586. doi: 10.3799/dqkx.2017.045

Citation:

Wang Wei, Yang Xianghua, Ye Jiaren, Wang Qingbin, Zhu Hongtao, Li Huan, 2017. Characterization and Controlling Factors of Sandstone Reservoirs in Basalt Development Areas: An Example from Comparison between BZ34-9 and KL6 Areas in South of Bohai Sea. Earth Science, 42(4): 570-586. doi: 10.3799/dqkx.2017.045

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Characterization and Controlling Factors of Sandstone Reservoirs in Basalt Development Areas: An Example from Comparison between BZ34-9 and KL6 Areas in South of Bohai Sea

doi: 10.3799/dqkx.2017.045

Wang Wei^{1,2
,},
Yang Xianghua^{1,2
,
,},
Ye Jiaren^1,2,
Wang Qingbin³,
Zhu Hongtao^1,2,
Li Huan³

1.
Key Laboratory of Tectonics and Petroleum Resources of the Ministry of Education, China University of Geosciences, Wuhan430074, China
2.
Faculty of Earth Resources, China University of Geosciences, Wuhan430074, China
3.
Tianjin Branch, CNOOC Ltd., Tianjin300452, China

Received Date: 2016-10-29
Publish Date: 2017-04-15

Abstract

Abstract

BZ34-9 area and KL6 area are located in the north and south of Laibei low uplift, respectively in south of Bohai Sea. The characteristics of the sandstone reservoirs in the two areas are of great differences in spite of the similar background of Cenozoic basalt development which has been proven by drilling. The contrastive studies on structural background, temporal-spacial distribution of basalt, sedimentary system and reservoir development have been taken combined with the analytical methods of 3-D seismic data, well log, casting thin section observation, SEM, BSE and X-ray diffraction. For the BZ34-9 area, braided river deltas were deposited on a gentle slope at low depositional rates. Syndepositional basalt flows occur in the upper and lower parts of the sand body and high-quality sandstone reservoirs are characterized by dolomite coats, zeolite cementation and dissolution, and mixed-layer clay coats, which collectively had a positive impact on the reservoir quality.By contrast, the KL6 area was situated on a steep slope and fan delta deposition occurred at a high rate. The Neogene basalt focused on the middle of the basin and had limited influence on the sandstone reservoirs which is characterized by abundant kaolinite and carbonate cementation. The Oligocene strata of KL6 area which situated near Tan-Lu fault zone has been greatly influenced by the Neogene basalt activities during the diagenesis stages. The magma and hydrothermal activity caused recrystallization of siderite, sericitization and prevailing precipitation of ferrodolomite. The basalt influence on the sandstone reservoirs are controlled by the time of eruption, source supply and the configuration of sandbody and basalt.
- basalt,
- sandstone reservoir,
- reservoir characteristics,
- BZ34-9 area,
- KL6 area,
- stratigraphy,
- petroleum geology

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References(73)

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沈阳化工大学材料科学与工程学院沈阳 110142

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Characterization and Controlling Factors of Sandstone Reservoirs in Basalt Development Areas: An Example from Comparison between BZ34-9 and KL6 Areas in South of Bohai Sea

doi: 10.3799/dqkx.2017.045

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