摘要
本文通过对方正地区所发现的负花状构造及其有关构造运动形迹分析的基础上，进一步提出方正断陷是走滑—拉分形成的断陷盆地。并从动力学、构造学等方面对其形成机制进行了分析探讨。
Based on the negative flower shaped structure and its relative structural movement track in Fangzheng area,this paper suggests that Fangzheng Rift is a rifted basin formed by strike slip pull apart.It discusses its formation mechanism with respect to dynamics and structures.
出处
《大庆石油地质与开发》
CAS
CSCD
北大核心
1997年第2期17-19,共3页
Petroleum Geology & Oilfield Development in Daqing
关键词
断裂带
方正断陷
动力学机制
断层
Fracture belt,Flower shaped structure,Strike slip pull apart basin,Fangzheng Rift
