赣北彭山-坳下矿集区地质特征与成矿预测  

Geological characteristics and mineralization prediction of the Pengshan Aoxia ore concentration area in northern Jiangxi

作　　者：谭荣 黄群 徐先宇 余振东 TAN Rong;HUANG Qun;XU Xian-yu;YU Zhen-dong(The Third Geological Brigade of Jiangxi Geological Bureau,Jiujiang 332100,China)

机构地区：[1]江西省地质局第三地质大队,江西九江332100

出　　处：《世界有色金属》2024年第23期46-48,共3页World Nonferrous Metals

摘　　要：本文将通过分析区内典型矿床(彭山锡铅锌矿床、潭里夏萤石锡铜矿床、坳下萤石铜铅锌矿床等)成矿地质、构造、岩浆岩、地球物理资料相结合来综合研究彭山地区的地质构造特征及其构造控矿规律,解剖本区构造对成矿作用影响、总结成矿规律。This article will comprehensively study the geological structural characteristics and ore controlling laws of the Pengshan area by analyzing the ore-forming geology,structure,magmatic rocks,and geophysical data of typical deposits in the area(Pengshan tin lead zinc deposit,Tanlixia fluorite tin copper deposit,Aoxia fluorite copper lead zinc deposit,etc.),dissecting the influence of the local structure on mineralization,and summarizing the mineralization laws.

关 键 词：彭山地区 隐伏花岗岩体 构造控矿 成矿规律 

分 类 号：P618.2[天文地球—矿床学]