板块漂移与中国的大地构造演化及效应  

Plate shift and its bearings on the tectonic evolution and effects in China

作　　者：方道恕 

机构地区：[1]江西煤田地质普查综合大队,江西南昌330201

出　　处：《沉积与特提斯地质》2007年第3期90-93,共4页Sedimentary Geology and Tethyan Geology

摘　　要：地球南北半球大小的波动变化,导致了板块运动。板块构造分板块移动构造、板块碰撞构造和板内构造。石油生成于板块前缘增生带,赋存于板块碰撞隆起带两侧的盆地中。板块的移动、碰撞和板内层间滑导致了地震,中国境内可以划分两个地震带。The fluctuations in sizes of the Northern and Southern Hemispheres lead to the occurrence of plate movements. The plate tectonics comprise moving tectonics, collision tectonics and within plate tectonics. The hydrocarbon tends to be generated in the plate frontal accretionary zones and hosted in the basins along the collision uplift zones. The shift, collision and within plate intraformational gliding of plates may result in the occurrence of earthquakes. Two seismic zones may be recognized in China： eastern and western seismic zones.

关 键 词：板块构造 油气 地震效应 全球 

分 类 号：P541[天文地球—构造地质学]