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《Chinese Journal of Geology(Scientia Geologica Sinica)》 2008-04
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Permo-Carboniferous coal measures in the Qinshui Basin:High-resolution sequence stratigraphy and coal accumulating models

Shao Longyi1 Xiao Zhenghui2 Wang Hao1 Lu Jing1 Zhou Jun1(1.Department of Resources and Earth Sciences,China University of Mining and Technology,Beijing 100083;2.Hunan University of Science and Technology,Xiangtan,Hunan 411201)  
The Qinshui Basin in southeastern Shanxi Province is an important base for coalbed methane exploration and production in China.The methane reservoirs in this area are Carboniferous and Permian coals and their thickness are strongly controlled by the depositional environments and the sequence stratigraphic framework.This paper analyzed the high-resolution sequence stratigraphy of the Permo-Carbonifersous Taiyuan and Shanxi Formations.The accumulating models of the No.15 and No.3 coals,the major coals in the Qinshui Basin,in the context of sequence stratigraphy were discussed.Bounded by regional disconformity,transgression direction switching surface,the base of incised valley fill sandstone,facies-reversal surface and associated palaeosols,the coal measures were subdivided into 3 third-order composite sequences and 9 fourth-order sequences.The No.15 coal of the Taiyuan Formation was formed in the barrier-lagoon and offshore shelf settings and was developed at the transgressive surface of the composite sequence Ⅱ,where the lower peat accumulation rate was balanced by the slower accommodation creation rate.In contrast,the No.3 coal of the Shanxi Formation was formed in a fluvial-delta setting,and was developed at the maximum surface of the composite sequence Ⅲ,where the higher peat accumulation rate was balanced by the higher accommodation creation rate.The coal in the fourth-order sequence represented by "seat earth-coal-marine limestone" could be formed during the "lag time" of marine deposits,when development of balanced accommodation creation rates and peat accumulation rates might favor the accumulation of thick coals.
【Fund】: 国家973项目(编号:2006CB202202);; 国家自然科学基金项目(批准号:40172050 40672103)资助
【CateGory Index】: P539.2
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