南海南部地洼区新构造运动及其动力学机制  

THE PRELIMINARY ANALYSIS OF NEOTECTONIC MOVEMENT AND DYNAMIC EVOLUTION IN THE SOUTHERN DIWA REGION OF SOUTH CHINA SEA

作　　者：詹文欢[1] 刘以宣[1] 钟建强[1] 

机构地区：[1]中国科学院南海海洋研究所

出　　处：《大地构造与成矿学》1995年第2期95-103,共9页Geotectonica et Metallogenia

摘　　要：本文根据南海南部地洼区的岩石圈动力学环境，把本区新构造运动类型划分为拉张型、挤压型、平移剪切型和旋动型，并对其构造演化与动力学模式进行了初步分析。According to the environment of lithospheric dynamic in the southern Diwa of the South China Sea, the neotectonism is classified into divergence, convergence, strike-slip and gliding types. And its tectonic evolution and dynamic model of the southern Diwa region of the South China Sea is preliminarily discussed.

关 键 词：新构造运动 动力学 地洼区 南海 

分 类 号：P546[天文地球—构造地质学]