摘要
本文根据新近资料,在概述大别山周边地区中新生代陆相地层序列的基础上,着重就其接触关系、岩相特征、火山活动、物质来源等进行了构造分析,探讨周边盆地形成演化与大别山隆起的时空及物质补偿关系。
Based on the latest data,this paper has made a structural analysis of the contact relationship,petro-graphic characteristics, volcanic activity and material source of the Mesozocc and Cenozoic terrestrial strati-graphic sequences presented,and discussed the time-space and material compensatiOn relationships of themarginal basin’s formation and evolution with the rise of Dabie Mt。
出处
《安徽地质》
1995年第3期13-18,共6页
Geology of Anhui
关键词
中新生代
陆相地层
火山活动
大别山隆起
盆地构造分析
Mesozoic and Cenozoic,terrebtrial strata,volcanic activity,rise of Dabie Mt basinstructure analy