RELATIONSHIP BETWEEN DEPOSITIONAL SYSTEMSAND CHARACTERISTICS OF COALBED GAS
RESERVOIR AND ITS CAPROCK
Qin Yong Fu Xuehai Yue Wei in Dayang Ye JianpingJiao Sihong
①College of Mineral Resource and Environment Science, CUMT, Xuzhou 221008
②Exploration Bureau No.1, China Administration of Coal Geology, Handan 056000
The six fundamental conditions of the coal reservoir and its caprock assemblages with some regular occurrence in spacetime exist in China. The sealing capability of the shallow sea and barrier island system to coal reservoir is relatively high, that of the shallow sea and plane coast system becomes mostly poor, that of the littoral delta system is commonly good, that of the fluvial system is relatively good if the sedimentary unit is complete or very poor if the coal reservoir is directly overlaid by the channel or splay medium to coarsegrained sandstone, that of the lake system is sufficiently high, and that of the alluvial fan system is generally very poor. The relationship between the sedimentation and coalbedroof condition not only occurs regionally in the North and South China, but also controls the distribution of the coalbed methane content in some given coalfields or coal mining districts, which provide the important reference for the prediction of the gasbearing coalbeds.
About author: Qin Yong, born in 1957, graduated from China University of Mining and Technology in 1992, and obtained the Ph.D. degree. Now he is a professor of China University of Mining and Technology and is engaged in coalbed methane.
Cite this article:
. RELATIONSHIP BETWEEN DEPOSITIONAL SYSTEMSAND CHARACTERISTICS OF COALBED GAS
RESERVOIR AND ITS CAPROCK[J]. JOURNAL OF PALAEOGEOGRAPHY, 2000, 2(1): 77-84.
. RELATIONSHIP BETWEEN DEPOSITIONAL SYSTEMSAND CHARACTERISTICS OF COALBED GAS
RESERVOIR AND ITS CAPROCK[J]. JOPC, 2000, 2(1): 77-84.