摘要
断裂和断块构造是南海北部陆缘新生代构造作用的基本特征。通过对断裂、断块以及其他地质特征的分析，认为珠江口盆地属过渡陆缘张裂盆地，并初步建立该盆地的构造演化模式。
Structures of faults and fault-blocks are the basic characteristics of tectonism in the north continental margin of South China Sea in the Cenozoic. By analysis of the faults, fault-blocks and other geologic features, it is suggested that the Pearl River Mouth Basin is a rifting basin on the transiton (or sub-active)continental margin. And a tectonic evolution model of the basin is preliminarily constructed.
出处
《海洋湖沼通报》
CSCD
北大核心
1994年第1期1-8,共8页
Transactions of Oceanology and Limnology
关键词
珠江口盆地
断裂
断块
盆地演化
Pearl River Mouth Basin, fault, fault-block, basin evolution, continental margin
