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作 者:石显耀[1] 曹代勇[1] 林玉成[2,3] 郑志红[1]
机构地区:[1]中国矿业大学煤炭资源与安全开采国家重点实验室,北京100083 [2]中国地质大学(北京),北京100083 [3]云南省煤田地质局,云南昆明650034
出 处:《中国煤炭地质》2009年第12期24-27,33,共5页Coal Geology of China
基 金:煤炭资源与安全开采国家重点实验室自主研究课题(SKLCRSM08B01);云南省煤炭及煤层气资源潜力评价(资[2008]02-01-25)
摘 要:运用构造控煤分析方法,根据后期控煤构造几何形态特征及形成机制,将滇东控煤构造划分为4大类(褶皱断裂组合、逆冲断裂组合、伸展构造组合和反转构造组合)11种控煤构造样式,其形成机制主要以挤压作用为主,辅以局部的拉张或走滑作用,在一些地区还存在因局部应力场改变而产生的变形。煤系赋存特征与控煤构造样式关系密切。以逆冲断裂组合为主的控煤构造样式,其煤系受构造破坏显著,煤系赋存范围较小;以褶皱断裂组合为主的控煤构造样式,其煤系赋存稳定,可形成大面积开发区块。Using the structural coal-control analytical method, according to the geometry of the succeeding coal-control structural features and formation mechanism in the Eastern Yunnan, the coal-control structural patterns were classified into four main combination types: fold and fault, reverse thrust, extensional structure and inversion structure, then subdivided into eleven coalcontrol structural patterns. The formation mechanism is mainly compressions, complemented by local extensional or strike-slip actions, in some places existed deformations generated by local stress field changing. The relation between coal measures hosting features and coal-control structural pattern is very close. When the reverse thrust combination is the main coal-control structural pattern, coal measures are obviously destructed by structures and only have smaller hosting extent; while the fold and fault combination is the main pattern, coal measures hosting is stable and may form large area exploitable blocks.
分 类 号:P618.110.2[天文地球—矿床学]
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