四川盆地川中地区盐亭-潼南海槽台缘带二叠系长兴组储层特征及成因探讨

李秋芬; 苗顺德; 李永新; 王铜山; 李军; 江青春; 翟秀芬

doi:10.3799/dqkx.2018.313

Volume 43 Issue 10

Oct. 2018

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Article Navigation > Earth Science > 2018 > 43(10): 3553-3567

Li Qiufen, Miao Shunde, Li Yongxin, Wang Tongshan, Li Jun, Jiang Qingchun, Zhai Xiufen, 2018. Reservoir Characteristics and Genesis of the Changxing Formation on the Margin of Yanting-Tongnan Trough, Central Sichuan Basin. Earth Science, 43(10): 3553-3567. doi: 10.3799/dqkx.2018.313

Citation:

Li Qiufen, Miao Shunde, Li Yongxin, Wang Tongshan, Li Jun, Jiang Qingchun, Zhai Xiufen, 2018. Reservoir Characteristics and Genesis of the Changxing Formation on the Margin of Yanting-Tongnan Trough, Central Sichuan Basin. Earth Science, 43(10): 3553-3567. doi: 10.3799/dqkx.2018.313

Citation:

Li Qiufen, Miao Shunde, Li Yongxin, Wang Tongshan, Li Jun, Jiang Qingchun, Zhai Xiufen, 2018. Reservoir Characteristics and Genesis of the Changxing Formation on the Margin of Yanting-Tongnan Trough, Central Sichuan Basin. Earth Science, 43(10): 3553-3567. doi: 10.3799/dqkx.2018.313

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Reservoir Characteristics and Genesis of the Changxing Formation on the Margin of Yanting-Tongnan Trough, Central Sichuan Basin

doi: 10.3799/dqkx.2018.313

1.
Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, China
2.
CNOOC Research Institute Co. Ltd., Beijing 100028, China

Received Date: 2018-04-11
Publish Date: 2018-10-20

Abstract

Abstract

The Permian Changxing Formation is considered as one of the key exploration strata in Sichuan Basin, which develops high-quality reef-bank reservoirs. At present, there is a lack of study on the reservoir characteristics and formation. Based on the study of regional geology, rock characteristic analysis, microscopic identification, cathodoluminescence image detection, combined with determinations of trace elements and isotopes such as Sr, Fe, Mn and C, O, Sr, the petrological and geochemical characteristics of reef-shoal reservoirs on the margin of the Yanting-Tongnan trough are systematically investigated in order to reveal the genesis of the reservoir. The reef-shoal complexes are regularly distributed in the central part of Sichuan under the control of the platform margin of Yanting Tongnan trough. The reefs are mainly distributed in the Guang'an-Gongshanmiao platform margin, east of the trough, with bioclastic shoal dolostone in the reef-shoal complex as the main reservoir rock. The porosity types of the shoal reservoir consist mainly of intergranular pore and bio-framework pore with high dolomitization degree. The bioclastic dolostone is thin and widely distributed. In comparison, bioclastic shoal rather than the reefs is developed in the western side of the trough, and the bioclastic limestone is the main reservoir rock with dissolved intergranular pores, intercrystalline pores and dissolved fractures. Despite its thin single layer, the cumulative thickness of the reservoir is large and its distribution is wide. It was indicated that buried dolomitization is the main origin of dolomite reservoir in Yanting-Tongnan area, and the seawater sealed in Changxing Formation during burial period which is mixed by meteoric water and compacted porewater possibly from the bottom of Feixianguan Formation shales are the mainsources of the dolomitization fluids. Regional exposure in the late stage of Changxing formation carbonate sedimentation and buried karst are the main reasons for the formation of karst reservoirs. The high quality reservoirs in Yanting-Tongnan trough are controlled by the platform margin zone, buried dolomitization, exposure dissolution during the end of Changxing period and buried karst. And the reservoirs are supposed to be effective reservoirs due to the large scale of their large cumulative thickness and wide distribution.
- Yanting-Tongnan trough,
- Changxing Formation,
- dolomitization,
- genetic model,
- petroleum geology

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References(70)

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