沁水煤田南部走滑断裂系统构造背景分析  

Analysis of Southern Qinshui Coalfield Strike-slip Fault System Tectonic Background

作　　者：郑翔天[1] 刘建军 王彦春[1] 路璐 

机构地区：[1]中国地质大学(北京)地球物理与信息技术学院,北京100083 [2]中国石油华北油田公司勘探开发研究院,河北任丘062552

出　　处：《煤炭技术》2016年第1期125-127,共3页Coal Technology

基　　金：国家"十二五"油气田及煤层气科技重大专项专题(2011ZX05033-004)

摘　　要：沁水煤田位于华北陆块的北部,研究区为盆地南部区域处于秦岭-大别山造山带与太行山构造带交接形成钝角的一侧。经过对野外露头资料、井下资料整理,找到盆地内发育的隐形走滑断裂带,确定了盆地的走滑构造模式,期望对区域煤层气勘探有指导意义。Qinshui coalfield is located in the north of North China landmass, research area is in the southern part of the basin. Through the systematic research of seismic profiles, outcrop data, found the appearance of strike-slip faults. Confirmed the strike＇slip System background of the coalfield. Expect to have guiding significance for the coalbed methane gas exploration in the area.

关 键 词：沁水盆地 南部 走滑断裂 构造发育史 

分 类 号：TD82[矿业工程—煤矿开采] TD166[矿业工程—矿山开采]