摘要
从遥感地质角度，结合地质、地貌来研究东北地区新生代地壳水平运动特征、规律。东北新生代地壳水平运动表现为水系变形、山体错移、新构造被错断、地质体错移变形等。呈现出其运动的广泛性、协调性、多期性、继承性和持续性。该区的应力场在新生代期间多次改变，并控制了主要断裂的活动方式。
The neotectonic movements in Northeast China are very intense,but theresearch papers on horizontal crust movements are few. By remote sensing analysis and in combination with the data of geology and geomorphology,we discussed thecharacteristics and regularity of Cenozoic horizontal crust movements in Northeastchina.The Cenozoic horizontal crust movements are shown by offset river and mountainsystems,neotectonics and geological bodies and exhibit the characteristics ofextensiveness,coordination,polycycle,inheritance and continuity,The stress field of thearea changed many times during Cenozoic and controlled the active styles of main faults.
关键词
遥感图像
新生代
地壳运动
Northeast China,Cenozoic,horizontal movement
