大同C-P煤盆地构造形式及成因分析  

Tectonic Form and Genesis Analysis of Datong C-P Coal Basin

作　　者：李亚奎 陈继福[1] 赵亮 安律宁 董广铭 LI Ya-kui;CHEN Ji-fu;ZHAO Liang;AN Lyu-ning;DONG Guang-ming(School of Coal Engineering,Shanxi Datong University,Datong Shanxi,037003)

机构地区：[1]山西大同大学煤炭工程学院,山西大同037003

出　　处：《山西大同大学学报（自然科学版）》2022年第4期100-104,共5页Journal of Shanxi Datong University(Natural Science Edition)

摘　　要：介绍了大同C-P煤盆地的构造轮廓和构造特征,分析了煤盆地的构造形式及成因,结果表明:燕山运动控制了NE向和NNW向的压性构造,喜马拉雅运动使得断裂构造性质发生了压性、张性的转换。同时,说明了后期构造变化对大同C-P煤层的影响。This paper mainly introduces the tectonic outline and structural characteristics of Datong C-P coal basin.The tectonic forms and genesis of the coal basin are analyzed.The results show that Yanshan movement controlled the NE and NNW compressive structures,and Himalayan movement caused the transformation of compressive and tensile properties of fault structures.At the same time,the influence of late tectonic changes on Datong C-P coal seam is explained in order to guide the construction and production of coal mines.

关 键 词：大同C-P煤盆地 构造形式 后期构造变化 

分 类 号：P5422[天文地球—构造地质学]