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滇西南翁孔坝铜多金属矿床火山岩系地质特征及其与铜的成矿关系
引用本文:吴子卓,张艳,韩润生,王蝶,曾淑明,田映天.滇西南翁孔坝铜多金属矿床火山岩系地质特征及其与铜的成矿关系[J].矿床地质,2023,42(3):579-597.
作者姓名:吴子卓  张艳  韩润生  王蝶  曾淑明  田映天
作者单位:昆明理工大学 国土资源工程学院, 云南 昆明 650093;有色金属矿产地质调查中心 西南地质调查所, 云南 昆明 650093
基金项目:本文得到云南省万人计划“青年拔尖人才”(编号: YNWR-QNBJ-2019-157)、云岭学者(编号: 2014)、云南省矿产资源预测与评价工程实验室(编号: 2012)、云南省和昆明理工大学创新团队项目联合资助
摘    要:翁孔坝铜多金属矿床是近年来在澜沧江构造带南段的云县-景洪火山弧上新发现的铜多金属矿床,与中三叠世陆相火山岩系密切相关,且具有较大的找矿潜力。文章在野外详细调查的基础上,结合赋矿火山岩岩石学特征,对矿区内火山岩系进行了系统研究,将其细分为5个喷发旋回,9个岩性段(T2s3-1~T2s3-9),认为该矿床具有火山沉积-成岩成矿期和改造成矿期两期成矿作用,为陆相火山沉积-改造型铜多金属矿床。其中,火山岩成矿作用为成矿提供了物质来源,具有明显的岩性/岩相组合控矿特征,笔者综合认为该套火山岩系是矿床主要的控矿因素之一,进而初步建立了其与铜成矿的“时-空-成因”关系图。

关 键 词:地质学  火山岩系  地质特征  成岩与成矿作用  民乐铜矿  翁孔坝铜矿  滇西南
收稿时间:2022/8/26 0:00:00
修稿时间:2023/5/15 0:00:00

Geological characteristics of volcanic series and their relationships with copper mineralization at Wengkongba copper polymetallic deposit, Southwest Yunnan Province
WU ZiZhuo,ZHANG Yan,HAN RunSheng,WANG Die,ZENG ShuMing,TIAN YingTian.Geological characteristics of volcanic series and their relationships with copper mineralization at Wengkongba copper polymetallic deposit, Southwest Yunnan Province[J].Mineral Deposits,2023,42(3):579-597.
Authors:WU ZiZhuo  ZHANG Yan  HAN RunSheng  WANG Die  ZENG ShuMing  TIAN YingTian
Institution:Faculty of Land Resources Engineering, Kunming University of Science and Technology, Kunming 650093, Yunnan, China;Southwest Institute of Geological Survey, Geological Survey Center for Non-Ferrous Mineral Resources, Kunming 650093, Yunnan, China
Abstract:The Wengkongba copper deposit is a newly discovered copper polymetallic deposit in the Yunxian-Jinghong volcanic arc of the southern section of the Lancang River tectonic belt. It is closely related to Middle Triassic continental volcanic series and has great prospecting potential. Based on detailed field investigation and petrological characteristics of the ore-bearing volcanic rocks, this paper makes a systematic study on the volcanic rock series of the deposit and recognizes that the host rocks can be subdivided into 5 eruptive cycles and 9 lithologic sections(T2s3-1~T2s3-9). It is considered that the deposit has two stages of mineralization, namely volcanic depositiondiagenetic mineralization period and reformed mineralization period. It is a continental volcanic sedimentarymodified copper polymetallic deposit. Among them, volcanic mineralization provides material source for mineralization and has obvious lithology/lithofacies combination ore-controlling characteristics. The author comprehensively considers that the volcanic series is one of the main ore-controlling factors of the deposit, and then preliminarily establishes the "time-space-genesis" relationship between the volcanic series and copper mineralization.
Keywords:geology  volcanic series  geological characteristics  diagenesis and metallogenesis  Minle copper deposit  Wengkongba copper deposit  southwest Yunnan Province
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