摘要
西藏日土县埃永错地区发育自北向南的推覆构造,发育加木久-宋巴-狼当和种木干-祝若南4396高-沙尔多垄-狼当两条逆冲推覆断裂带,形成一系列构造窗和飞来峰构造。逆冲推覆构造形成于始新世之后,推覆体推覆距离大于3km。
The from north to south nappe structures developed in the Aiyongcuo area of Ritu County,Tibet,comprise two overthrust nappe fault zones as the Jiamuiu-Songba-Langdang one and the Zhongmugan-Zhuruonan 4396m highland-Shaerduolong-Langdang one,forming a series of tectonic window and klippe structures.The overthrust structure was formed after the Eocene epoch and its nappes have overthrust distances of more than 3 km.
作者
肖业斌
饶仁堂
邓必荣
XIAO Yebin;Rao Rentang;Deng Birong(Geological Survey of Jiangxi Province,Nanchang 330030,China;Institute of Basic Surveying and Mapping of Jiangxi Province,Nanchang 330209,China)
出处
《四川有色金属》
2019年第3期44-46,共3页
Sichuan Nonferrous Metals
基金
中国地质调查局工作项目(编号1212010730109 1212010818032)
关键词
形成时代
推覆构造
埃永错地区
西藏日土县
forming age
nappe structure
the Aiyongcuo area
Ritu County of Tibet
