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.
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.
出处
《华南师范大学学报（自然科学版）》
CAS
1989年第1期44-50,共7页
Journal of South China Normal University(Natural Science Edition)
关键词
断层
构造岩
中生代
主断裂面
瘦狗岭
广州
Fault
tectomteY Mesozonic
major fault, plang
Sougouling
Guangzhou
