Ore-controlling effect of structure and distribution of deep rock mass on Pb-Zn deposit in Qingchengzi ore concentration area,Liaoning

作     者：NIU Mingxuan YU Yunliang TIAN Liya NIU Wenqing XU Haibo NIU Mingxuan;YU Yunliang;TIAN Liya;NIU Wenqing;XU Haibo

作者机构：College of Earth SciencesJilin UniversityChangchun 130026China 

出 版 物：《Global Geology》 (世界地质（英文版）)

年 卷 期：2020年第23卷第2期

页      面：92-98页

学科分类：081901[工学-采矿工程] 0819[工学-矿业工程] 08[工学] 

基　　金：Supported by the National Science Foundation for Distinguished Young Scholars of China(No.41502309) 

主　　题：fault structure lead-zinc deposit profile inversion Qingchengzi Liaoning 

摘      要：Qingchengzi ore concentration area in Liao-Ji rift is an important lead-zinc ore area of China,and the deep prospecting in this area has great *** on the spatial occurrence of ore bodies the Pb-Zn deposit can be divided into three types:layered,vein-shaped and *** deep geological conditions in this area are deduced by analyzing the tectonic evolution process and rock mass gravity *** tectonic evolution of Liao-Ji rift can be divided into three stages:Paleoproterozoic extension period,Mesoproterozoic compression period and Mesozoic reactivation *** magmatic activities in the Indosinian epoch led to the distribution pattern of the present *** to the gravity inversion,Shuangdinggou-and Xinling rock masses on the north and south sides of the mining area are connected in the *** connected rock body might be distributed in the entire mining *** rock mass may be a branch extending from Shuangdinggou rock mass along the northeast trending fault,the connected rocks provide magmatic hydrothermal fluid for the final,folds and faults result in different types of ore body shapes.