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中国大陆现今地壳垂直运动概貌及其地球动力学的某些特征
引用本文:杨国华,巩曰沐.中国大陆现今地壳垂直运动概貌及其地球动力学的某些特征[J].测绘学报,1994,23(3):184-189.
作者姓名:杨国华  巩曰沐
作者单位:国家地震局第一地形变监测中心!天津300180(杨国华,王若柏,孙汉荣),国家地震局综合观测队!北京100039(巩曰沐)
摘    要:本文根据均衡理论,编绘了我国大陆地区现今地壳垂直运动速率图(不包括台湾、海南等岛屿)。结果显示,我国大陆地区的运动特征为“南和或北降”、“东弱西强”;且明显地受印度板块和太平洋板块所控制,以印度板块的作用为最强烈。

关 键 词:地壳运动  地球动力学  中国大陆

RECENT VERTICAL CRUSTAL MOVEMENTSIN THE MAINLAND OF CHINA AND THEIRGEODYNAMIC FEATURES
Yang Guohua,Wang Ruobai,Sun Hanrong.RECENT VERTICAL CRUSTAL MOVEMENTSIN THE MAINLAND OF CHINA AND THEIRGEODYNAMIC FEATURES[J].Acta Geodaetica et Cartographica Sinica,1994,23(3):184-189.
Authors:Yang Guohua  Wang Ruobai  Sun Hanrong
Abstract::Based on the concept of flux-isostatic datum, maps showing the rate of recent vertical crustal movements of China mainland (excluding Taiwan, Hai nan and subordinate islands) have bee'n compiled. As seen in the maps, the overall features of the vertical movements are: uplifting in the south and subsi ding in the north, strong in the west and weak in the east. These movements are apparently constrained by Indian and Pacific plates, the former plays a dominant role.
Keywords::mainland of China  vertieal crustal movement  geodynamicsfeatures
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