广西龙殿铜铅锌重晶石矿地质特征及成矿规律  

GEOLOGICAL CHARACTERISTICS AND METALLOGENIC LAWS OF THE LONGDIAN COPPER-LEAD-ZINC-BARITE DEPOSIT IN GUANGXI

作　　者：蒲利国 杨昌华 姜永果 张贤峰 周宇 朱迪 PU Li-guo;YANG Chang-hua;JIANG Yong-guo;ZHANG Xian-feng;ZHOU Yu;ZHU Di(Geological Exploration Institute,Yunnan Bureau of Nonferrous Geology,Kunming 650216;Geological,Geophysical and Chemical Exploration Institute,Yunnan Bureau of Nonferrous Geology,Kunming 650216)

机构地区：[1]云南省有色地质局地质勘查院,云南昆明650216 [2]云南省有色地质局地质地球物理化学勘查院,云南昆明650216

出　　处：《云南地质》2024年第S01期302-308,共7页Yunnan Geology

摘　　要：龙殿铜铅锌重晶石多金属矿区位于大瑶山西侧成矿带北部。矿化严格受构造破碎带控制,矿体(化)主要产出于断裂破碎带,矿体形成时代为印支-燕山早期,中-低温热液型矿床。通过对该区成矿地质特征及成矿规律的研究,对该区后续开展地质勘查工作,实现资源储量的突破,具有重要指导意义。TheLongdian copper-lead-zinc-barite polymetallic mining area is located in the north of the western Dayaoshan metallogenic belt.Mineralization is strictly controlled by structural fracture zones.The ore bodies(mineralization),formed during the Indosinian-Early Yanshan period,are mainly hosted in fractured zones.The deposit is a middle-low temperature hydrothermal deposit.Researches on the geological characteristics and metallogenic laws of this area provide significant guidance for subsequent geological exploration work and breakthroughs in resource reserves.

关 键 词：地质特征 控矿因素 成矿规律 龙殿铜铅锌重晶石矿 广西象州 

分 类 号：P618.41[天文地球—矿床学] P618.42[天文地球—地质学] P618.43