摘要
Objective The Early Paleozoic tectonic events such as oceanic subduction and collision-orogeny in the North Altyn have been extensively studied.The Lapeiquan Group,distributed in the Hongliugou ophiolite melange belt(Fig.1),was interpreted to form along with the Ordovician Caledonian tectonic events.Based on few evidence of macrofossils。
基金
This work was financially supported by the Open Fund(grant No.PLC20180505)
of State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology and the National Natural Science Foundation of China(grant No.41502116).
