Deformation of the Shirenshan Block in the North Qinling  

作　　者：WANG Jingya REN Shenglian LI Jiahao LI Quanzhong SONG Chuanzhong LI Longmin LIN Shoufa HUANG Yonglong HAN Xu LI Zhenqiang 

机构地区：[1]Hefei University of Technology, Hefei 230009, Anhui, China [2]University of Waterloo, Waterloo, Ontario N2L 3G1, Canada [3]University of Science and Technology of China, Hefei 230026, Anhui, China

出　　处：《Acta Geologica Sinica(English Edition)》2017年第1期351-352,共2页地质学报（英文版）

基　　金：supported by the National Science Foundation of China (grants No.41272213 and 41572177)

摘　　要：Objective The Qinling orogenic belt is a typical complex continental orogenic belt which has experienced multiperiod tectonic evolution and where some important tectonic belts formed.The Luoluan fault is one of the most important belts,which is the boundary fault of the North China Plate and the Qinling orogenic belt.The Shirenshan block is located in the north section between Luanchuan and Fangcheng of the Luoluan fault.Objective The Qinling orogenic belt is a typical complex continental orogenic belt which has experienced multiperiod tectonic evolution and where some important tectonic belts formed.The Luoluan fault is one of the most important belts,which is the boundary fault of the North China Plate and the Qinling orogenic belt.The Shirenshan block is located in the north section between Luanchuan and Fangcheng of the Luoluan fault.

关 键 词：Deformation of the Shirenshan Block in the North Qinling 

分 类 号：P542[天文地球—构造地质学]