摘要
本文以１∶５万区调资料为基础，对大港周地区滑脱构造的层块特征、岩石力学性质及物性特征，主滑面及次滑面的基本特征作了较详细的描述，把本区滑脱构造归属为萍乡式（叠瓦式）。
Based on new data from 1∶50 000 regional survey,this paper gives a detailed description on the layer and block features of decollement structure,mechanical and physical properties of rocks and the major and subordinate sliding planes in the Dagangzhou area.The decollement structure of this area has been attributed to the Pingxiang style which is characterized by imbricate arrangement,and its origin has been discussed.
出处
《江西地质》
1997年第1期40-45,共6页
Jiangxi Geology
关键词
滑脱构造
构造样式
成因构式
大港周
彭泽
decollement structure,structural style,genetic structural style,Dagangzhou,Pengze
