摘要
龙门山中－ 南段前陆盆地变形区、后山褶皱推覆带和滑覆飞来峰构成了本区的基本构造格局，它是在古生代扬子板块西缘稳定大陆边缘陆棚沉积建造的基础上经历印支运动以来多次变形改造的结果。
The foreland basin deformation area, metamorphic fold nappe and gliding klippes constitute the structural framework in the Middle-South section of the Longmen Mountains. It was formed from the shelf sedimentary formation of Paleozoic passive continental margin in the west Yangtse platform by multiple deformation since the Indo-China movement.
出处
《矿物岩石》
CAS
CSCD
北大核心
1999年第3期82-85,共4页
Mineralogy and Petrology
基金
国土资源部"九五"1:50000 区调研究成果
关键词
龙门山
构造格局
地质演化
前陆盆地
推覆构造
Longmen Mountains structural framework geological evolution foreland basin nappe klippe
