构造和古地理控制下的碳酸盐岩储集体旋回和集群性探讨:以四川盆地为例

邢凤存; 胡华蕊; 侯明才; 陆永潮

doi:10.3799/dqkx.2018.310

Volume 43 Issue 10

Oct. 2018

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Article Navigation > Earth Science > 2018 > 43(10): 3540-3552

Xing Fengcun, Hu Huarui, Hou Mingcai, Lu Yongchao, 2018. Carbonate Reservoirs Cycles and Assemblages under the Tectonic and Palaeogeography Control: A Case Study from Sichuan Basin. Earth Science, 43(10): 3540-3552. doi: 10.3799/dqkx.2018.310

Citation:

Xing Fengcun, Hu Huarui, Hou Mingcai, Lu Yongchao, 2018. Carbonate Reservoirs Cycles and Assemblages under the Tectonic and Palaeogeography Control: A Case Study from Sichuan Basin. Earth Science, 43(10): 3540-3552. doi: 10.3799/dqkx.2018.310

Citation:

Xing Fengcun, Hu Huarui, Hou Mingcai, Lu Yongchao, 2018. Carbonate Reservoirs Cycles and Assemblages under the Tectonic and Palaeogeography Control: A Case Study from Sichuan Basin. Earth Science, 43(10): 3540-3552. doi: 10.3799/dqkx.2018.310

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Carbonate Reservoirs Cycles and Assemblages under the Tectonic and Palaeogeography Control: A Case Study from Sichuan Basin

doi: 10.3799/dqkx.2018.310

1.
State Key Laboratory of Oil and Gas Reservoir Geology, Chengdu University of Technology, Chengdu 610059, China
2.
Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China
3.
Faculty of Earth Resource, China University of Geosciences, Wuhan 430074, China

Received Date: 2018-05-21
Publish Date: 2018-10-20

Abstract

Abstract

The oil/gas exploration of marine carbonate rocks in Sichuan basin has achieved a lot of breakthroughs. Several large gas field clusters have been gradually presented, and have shown the clumped distribution characteristics of carbonate reservoirs, while the assemblage structure of the reservoirs and its spatial and temporal distribution remain to be further discussed. Based on previous studies, combined with the comprehensive research on marine carbonate reservoirs in Sichuan Basin, the types, texture, and major controlling factors of carbonate cycles and assemblages under the control of tectonic and paleogeography have been systematically studied. Limited by stable clastic rock strata and large unconformity surfaces, eight carbonate cycles are divided in this paper, and each cycle has different reservoir compositions.The cycles include dolomite favorable for reservoirs such as ones of Sinian to Lower Ordovician, and Middle Permian to Middle Triassic.Combined with the tecotonic space-time distribution, and lithofacies paleography of reservoirs, carbonate rock assemblages are divided into several vertical cycles including:(1) stable platform edge reefs and shoals reservoirs on the edge of Upper Yangtze plate, (2) supergene karstification and grain beach dolomite around continuous migration paleo-uplift, (3) algal dolomite and intra-platform shoals under the background of tidal flat in the plate, (4) reef and beach dolomite reservoirs on the both sides of platform margin and intra-platform depression controlled by faults in the plate, and (5) dense limestone and karst reservoirs of carbonate ramp. It is suggested that carbonate reservoirs assemblages are controlled by dolomite which has been protected by early oil and gas charging. Carbonate reservoirs assemblages are influenced by tectonics, sea-level, and lithofacies paleography. And other factors such as karst, TSR, and hot fluids etc. influence carbonate reservoirs in local area.
- carbonate reservoirs,
- reservoir assemblage,
- Craton,
- paleo-uplift,
- intracratonic sags,
- Paleozoic,
- Sichuan Basin,
- petroleum geology

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References(65)

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Carbonate Reservoirs Cycles and Assemblages under the Tectonic and Palaeogeography Control: A Case Study from Sichuan Basin

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