摘要
古鄱阳湖中生代盆地的研究表明,该盆地并不是简单的白垩纪盆地,而是历经多次构造旋回的复杂盆地。盆地多次成生、萎缩、上升,均是燕山运动的结果。
Reasearch of Mesozoic Basin in old Poyanghu showed that the basin underwent multiple complex tectonic cycles. The basin was first formed in the early Jurassic instead of the Cretaceous. It was the result of the Yanshan movement with multiple generation,shrinkage and uplifting.
出处
《资源调查与环境》
2003年第3期167-176,共10页
Resources Survey & Environment
基金
国家地调项目:田坂街、游城幅1:5万联测
关键词
充填序列
环境相
演化特征
中生代
古鄱阳湖盆地
filled sequence
environment facies
evolution characteristics
Mesozoic Era
Old Poyanghu
