| 台西南盆地晚新生代地质演化分析 |
| |
| 引用本文： | 钟建强,黄慈流,詹文欢.台西南盆地晚新生代地质演化分析[J].海洋科学,1994,18(4):34-38. |
| |
| 作者姓名： | 钟建强 黄慈流 詹文欢 |
| |
| 作者单位： | 中国科学院南海海洋研究所!广州510301 |
| |
| 摘 要： | 通过对构造沉降、断裂活动、岩浆活动、构造应力场等分析，认为台西南盆地晚新生代地质演化存在两个旋回，即渐新世－中中新世受南海扩张控制、陆缘主动裂陷－沉降旋回和晚中新世－第四纪受台湾弧－陆碰撞影响、陆缘被动拉张－活化旋回。
|
| 关 键 词： | 台西南盆地 地质演化 晚新生代 |
| 收稿时间： | 1993/4/25 0:00:00 |
GEOLOGIC EVOLUTION ANALYSE OF TAIXINAN BASIN IN LATE CENOZOIC ERA |
| |
| Zhong Jianqiang,Huang Ciliu and Zhan Wenhuan.GEOLOGIC EVOLUTION ANALYSE OF TAIXINAN BASIN IN LATE CENOZOIC ERA[J].Marine Sciences,1994,18(4):34-38. |
| |
| Authors: | Zhong Jianqiang Huang Ciliu and Zhan Wenhuan |
| |
| Abstract: | By analyses of characteristics of tectonic subisdence, fault activity, magmation, and tectonic stress field, it is suggested that there are two cycles of geologic evolution of Taixinan Basin in lute Cenozoic Era. One is the active rifting-subodence cycle of continental margin which be controled by the spreadig of South China Sea in Oligocene -Middle Miocene. The other is the negative rifting-reactivity cycle of continental margin which be influenced by the collison between the arc and the continental margin of Taiwan in Late Miocene-Quaternary. |
| |
| Keywords: | Taixinan Basin Continental margin Evolution |
| 本文献已被 CNKI 维普 等数据库收录！ |
| 点击此处可从《海洋科学》浏览原始摘要信息 |
| 点击此处可从《海洋科学》下载免费的PDF全文 |
