摘要
主要论述中生代晚期到新生代期间拉张应力作用下珠江口盆地的张裂和南海海盆的扩张,并根据拉张破裂理论论述它们之间的相互关系,进而探讨华南大陆边缘在这期间内产生上述形变的动力学机制。
Extension of Pearl River Mouth Basin and spreading in South China Sea Basin were illustrated in this paper. The relationship between the extension in Pearl River Mouth Basin and the spreading in South China Sea Basin was analysed on the theory of fracture. Furthermore, the dynamic mechanism in South China continental margin during Late Mesozoic to Cenozoic was discussed.
出处
《热带海洋》
CSCD
1992年第4期77-83,共7页
基金
中国科学院南海海洋研究所所长基金阶段成果
关键词
拉张应力
盆地
海盆
中生代
extensive stress, Pearl River Mouth Basin, South China Sea Basin, theory of fracture, dynamic mechanism
