陆东地区构造几何学和构造运动学分析  

TECTONOGEOMETRY AND TECTONOKINEMATICS ANALYSIS OF LUDONG AREA

作　　者：吴青鹏[1] 谭开俊[1] 牟中海[1] 王洪峰[1] 浦世照[2] 

机构地区：[1]西南石油学院资源环境学院,四川成都610500 [2]新疆油田分公司勘探开发研究院,新疆克拉玛依834000

出　　处：《西南石油学院学报》2004年第5期14-17,共4页Journal of Southwest Petroleum Institute

摘　　要：陆东地区构造几何学分析认为 :多期次、多类型、同生、早期右行、晚期左行是该区断裂的主要特征 ;构造运动学分析认为 :中海西期以来的各期构造运动直接控制了该区的沉积与构造演化特征 ,各期构造运动各具特色。通过研究还发现 。According to Tectonogeometry analysis of Ludong area,it is seen that the main characters of faulting in the area are the multi-phases,multi-types,dextrorotatory in the early stage,sinistral in the later stage; Tectonohnematlcs analysis of Ludong area indicates that every tectonic movement controlled directly the characters of sedimentation and evolution from the middle Hercynlan,and they had the features themselves.The compaction strength is larger In the east than In the west.

关 键 词：构造几何学 构造运动学 陆东地区 

分 类 号：P551[天文地球—构造地质学]