| 中生代晚期到新生代拉张应力下的华南大陆边缘 |
| |
| 引用本文： | 苏达权,夏斯高.中生代晚期到新生代拉张应力下的华南大陆边缘[J].热带海洋学报,1992(4). |
| |
| 作者姓名： | 苏达权 夏斯高 |
| |
| 作者单位： | 中国科学院南海海洋研究所，中国科学院南海海洋研究所 广州 510301，广州 510301 |
| |
| 基金项目： | 中国科学院南海海洋研究所所长基金阶段成果 |
| |
| 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。
|
| 关 键 词： | 拉张应力 珠江口盆地 南海海盆 破裂理论 动力学机制 |
EXTENSION IN SOUTH CHINA CONTINENTAL MARGIN FROM LATE MESOZOIC TO CENOZOIC |
| |
| SU Daquan XIA Sigao.EXTENSION IN SOUTH CHINA CONTINENTAL MARGIN FROM LATE MESOZOIC TO CENOZOIC[J].Journal of Tropical Oceanography,1992(4). |
| |
| Authors: | SU Daquan XIA Sigao |
| |
| Abstract: | 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. |
| |
| Keywords: | extensive stress Pearl River Mouth Basin South China Sea Basin theory of fracture dynamic mechanism |
| 本文献已被 CNKI 等数据库收录！ |
