摘要
文章从泥盆系、石炭系尤其是二叠系到下三叠统在中国东南部的展布、系统的沉积演变，联系到该阶段古特提斯洋对其影响和控制，提出了华南陆块东南部晚古生代—早三在世陆缘裂陷系发展的沉积构造模式。
Based on the distribution and depositional evolution of the Devonian, Carboniferous, and especially from Permian to Lower Triassic of southeast China, relating the effect and control of the Palaeotethys on them in these periods, the paper proposes the depositional and structural model for the development of the marginal rift system in the southeast of South China continental mass from later Palaeozoic to early Triassic age.
出处
《成都理工学院学报》
CSCD
1995年第1期52-59,共8页
Journal of Chengdu University of Technology
基金
地质行业基金
关键词
晚古生代
早三叠世
陆缘裂陷系
构造演化
southeast China
from later Palaeozoic to early Triassic
distal turbidite
marginal rift
