平庄盆地地质构造及演化特征  

Characters of geological structure and structural evolution of Pingzhuang basin

作　　者：王宇林[1] 何保[1] 姜志刚[1] 赵忠英[1] 

机构地区：[1]辽宁工程技术大学资源与环境工程学院,辽宁阜新123000

出　　处：《煤炭学报》2007年第10期1036-1040,共5页Journal of China Coal Society

基　　金：国家自然科学基金资助项目(50474010)

摘　　要：通过野外地质调查及煤田地质、石油地质信息的综合分析,揭示了平庄盆地的地质构造及演化特征.得出如下结论:八里罕拆离断裂是成盆的主控断裂;早期该盆地为地堑式盆地,中晚期演化为半地堑式盆地;挤压构造应力场导致了平庄裂陷盆地消亡;此后该区又经历了北北东向断裂左行走滑(形成了小型拉分盆地,将平庄盆地与相邻的元宝山盆地连通)以及形成北北西向褶皱的构造活动改造.Through field geological survey and comprehensive analysis of coal and oil geological information,the basin's characters of geological structure and structural evolution were revealed.The conclusions are as follows: the Balihan detachment fault was the main controlling fault;during the earlier period,Pingzhuang basin was a graben basin but in middle and later period,the basin became a semi-graben basin;the extrusing tectonic stress field made Pingzhuang rift basin died out;since then this area underwent str...

关 键 词：平庄裂陷盆地 构造格架 构造演化 拆离断层 走滑断层 

分 类 号：P542[天文地球—构造地质学]