全新世构造运动基本特征初探  

A Preliminary Discussion on Basic Features of the Holocene Tectonic Movement

作　　者：徐馨[1] 沈志达 

机构地区：[1]南京大学 [2]贵州省地质矿产局

出　　处：《贵州地质》1989年第2期140-152,共13页Guizhou Geology

摘　　要：全新世中全球地壳变动主要集中分布在环太平洋岸及南洋群岛经喜马拉雅山至地中海地带两个地区。构造运动特点主要为水平运动,次为垂直运动,其表现则以继承性、多类型的断裂活动,伴以地震、火山、地裂等运动。在晚更新世冰川覆盖区,全新世地壳变动则以冰川均衡运动为主要特征。The Holocene crustal movement of the earth mianly occured along the Pacific coast, on the Malay Archipelago and Malay Peninsula and in Indonesia, southeast Asia, the Himalayas and the Mediterranean. The features of the tectonic movement showed that the movement was mainly horizontal and secondly vertical, with fault activities in succession and different types, accompanied by seismic motion, volcanic activities and cracking activities, etc. In Late Pleistocene glacier-covering areas, the Holocene crustal movement mainly showed the features of glacial isostatic movement.

关 键 词：全新世 构造运动 

分 类 号：P546[天文地球—构造地质学]