四川盆地东部黄龙组碳酸盐岩储层沉积-成岩系统

文华国; 郑荣才; 沈忠民

doi:10.3799/dqkx.2011.012

Volume 36 Issue 1

Jan. 2011

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Article Navigation > Earth Science > 2011 > 36(1): 111-121

WEN Hua-guo, ZHENG Rong-cai, SHEN Zhong-min, 2011. Sedimentary-Diagenetic Systems of Carbonatite Reservoirs in the Huanglong Formation, Eastern Sichuan Basin. Earth Science, 36(1): 111-121. doi: 10.3799/dqkx.2011.012

Citation:

WEN Hua-guo, ZHENG Rong-cai, SHEN Zhong-min, 2011. Sedimentary-Diagenetic Systems of Carbonatite Reservoirs in the Huanglong Formation, Eastern Sichuan Basin. Earth Science, 36(1): 111-121. doi: 10.3799/dqkx.2011.012

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Sedimentary-Diagenetic Systems of Carbonatite Reservoirs in the Huanglong Formation, Eastern Sichuan Basin

doi: 10.3799/dqkx.2011.012

State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China

Received Date: 2010-07-10
Publish Date: 2011-01-01

Abstract

Abstract

The Huanglong Formation of Upper Carboniferous in eastern Sichuan basin, is the principal producing formation of natural gas pool. Based on the observation of cores, actual measurement of outdoors sections and analysis of thin section, and the data of well drilling, well logging, physical property analysis and X-diffraction analysis, we have studied the sedimentary-diagenetic system of carbonatite reservoirs in the Huanglong Formation, eastern Sichuan basin. It is believed that the Huanglong Formation mainly developed three facies belts, including sabkha, barrier coast and continental shelf, and particular palaeokarst facies. The types of reservoir rocks are mainly grain dolomite and dolomitic-karst breccia. The effective reservoir interspaces are mainly intercrystal pore and dissolved pore. The most important types of reservoir is cavity-seam. The beneficial localization for the development of reservoirs is the microtopography unit of hillsides and residual hills on sur-slope of palaeokarst. According to the studies above-mentioned, it is proposed that the sedimentary-diagenetic system has a good coupling relationship with reservoirs on time and space. The particles shoal of sedimentary microfacies controls the distribution of location regional of reservoirs. The diagenetic system of compaction-bittern of early-middle diagenetic stage, the diagenetic system of atmospheric water of paleo-hypergene stage and the diagenetic system of thermobaric-water of burial diagenetic stage contribute much to the development of goodness reservoirs.
- sedimentary facies,
- dolomitic,
- palaeokarst,
- carbonatite reservoirs,
- sedimentary-diagenetic system,
- Carboniferous,
- Huanglong Formation,
- eastern Sichuan basin

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Sedimentary-Diagenetic Systems of Carbonatite Reservoirs in the Huanglong Formation, Eastern Sichuan Basin

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