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.
出处
《大地构造与成矿学》
EI
CAS
CSCD
1995年第2期95-103,共9页
Geotectonica et Metallogenia
关键词
新构造运动
动力学
地洼区
南海
Neotectonic movement, dynamics, Diwa region, the southern part of the South China Sea
