| 珠江口盆地的构造特征与盆地演化 |
| |
| 引用本文： | 钟建强.珠江口盆地的构造特征与盆地演化[J].海洋湖沼通报,1994(1):1-8. |
| |
| 作者姓名： | 钟建强 |
| |
| 作者单位： | 中国科学院南海海洋研究所!广州51030 |
| |
| 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。通过断裂，断块以及其他地持的分析，认为珠江口盆地属过陆缘张裂盆地，并初步建立该盆地的构造演化模式。
|
| 关 键 词： | 珠江口盆地 断裂 断块 盆地演化 |
CHARACTERISTICS OF GEOLOGIC STRUCTURE AND BASIN EVOLUTION IN PEARL RIVER MOUTH BASIN |
| |
| Zhong Jianqiang.CHARACTERISTICS OF GEOLOGIC STRUCTURE AND BASIN EVOLUTION IN PEARL RIVER MOUTH BASIN[J].Transaction of Oceanology and Limnology,1994(1):1-8. |
| |
| Authors: | Zhong Jianqiang |
| |
| Abstract: | 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. |
| |
| Keywords: | Pearl River Mouth Basin fault fault-block basin evolution continental margin |
| 本文献已被 CNKI 维普 等数据库收录！ |
