| 对广州瘦狗岭断裂带特征的一些认识 |
| |
| 引用本文： | 龙志强,吴克刚.对广州瘦狗岭断裂带特征的一些认识[J].华南师范大学学报(自然科学版),1989,0(1):1. |
| |
| 作者姓名： | 龙志强 吴克刚 |
| |
| 作者单位： | 华南师范大学地理系
(龙志强)，华南师范大学地理系(吴克刚) |
| |
| 摘 要： | 广州瘦狗岭断层属广州—罗浮山大断裂带的西段,断层带内构造岩极为发育,可划分成七带,并有两个晚近时期形成的主断裂面,它是一个自中生代以来经受长期、多次活动的东西向大断层.
|
| 关 键 词： | 断层 构造岩 中生代 主断裂面 瘦狗岭 广州 |
A VIEW ON SOME CHARACTERISTICS OF SHOUGOULING FAULT BELT, GUANGZHOU |
| |
| Long Zhiqiang Wu Kegang.A VIEW ON SOME CHARACTERISTICS OF SHOUGOULING FAULT BELT, GUANGZHOU[J].Journal of South China Normal University(Natural Science Edition),1989,0(1):1. |
| |
| Authors: | Long Zhiqiang Wu Kegang |
| |
| Institution: | Geog. Dept. |
| |
| Abstract: | Shougouling Fault in Guangzhou is the west part of Guangzhou-Luofushan Major Fault Belt. It is characterized by well developed tectonite belt which could be divided into seven different belts, and formed into two major fault planes in neoid period. This east-to-west fault belt has been long-term and polygene active since Mesozonic. |
| |
| Keywords: | Fault tectomteY Mesozonic major fault plang Sougouling Guangzhou |
| 本文献已被 CNKI 等数据库收录！ |
| 点击此处可从《华南师范大学学报(自然科学版)》浏览原始摘要信息 |
| 点击此处可从《华南师范大学学报(自然科学版)》下载免费的PDF全文 |
