摘要
本文探讨了大庆长垣的形成机制，认为：大庆长垣主体是典型的正向反转构造，反转期的分界面是泉头组与青山口组分界面，松辽盆地内部地体的活动是挤压力源的重要组成部分。
This paper discusses the forming mechanism of Daqing placanticline,drawing theconclusion that,the mainbody of Daqing placanticline is a typical forward reversal structure;boundary of reversal period is that of Quantou and Qingshan formations;and interior activi-ties of Songliao basin are important forming part of source of compressional force.
出处
《大庆石油地质与开发》
CAS
CSCD
北大核心
1995年第2期1-2,共2页
Petroleum Geology & Oilfield Development in Daqing
关键词
松辽盆地
大庆长垣
反转构造
逆断层
形成
Songliao basin,Daqing placanticline,Reversal structure,Thrust,Forming.
