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湖南省留书塘铅锌矿床S、Pb同位素特征及意义

程顺波 吴志华 刘重芃 刘阿睢 马丽艳 卢友月

地质通报2017,Vol.36Issue(5):846-856,11.
地质通报2017,Vol.36Issue(5):846-856,11.

湖南省留书塘铅锌矿床S、Pb同位素特征及意义

Sulfur and lead isotope geochemistry of the Liushutang lead-zinc deposit in Hu'nan Province and its significance

程顺波 1吴志华 2刘重芃 3刘阿睢 1马丽艳 2卢友月1

作者信息

  • 1. 中国地质调查局武汉地质调查中心,湖北武汉430205
  • 2. 中国地质调查局花岗岩成岩成矿地质研究中心,湖北武汉430205
  • 3. 湖南省地质矿产勘查开发局四一七地质队,湖南衡阳421001
  • 折叠

摘要

Abstract

The discovery of the Liushutang lead-zinc deposit is one of the major breakthroughs of prospecting in the Nanling metal?logenic belt in recent years. The lead-zinc lodes are strictly controlled by the shattered fracture zones along the western margin of Hengyang basin. Field observation shows that the related mineralization can be divided into three stages of quartz-pyrite, quartz-sphalerite-galena and barite. In this paper, systematic research on S, Pb isotopes based on different stages of ores were conducted to explain the origin of ore-forming materials and ore genesis. The result shows that sulfur isotopes of 17 sulfide samples vary in a wide range (δ34S value being-12.8‰~4.6‰) with a dynamic evolution of gradual increasing of δ34S values from early to late. This can be probably explained by a mixing process of organic sulfur (~-13‰) and magmatic sulfur (~5‰). Sulfur of latest barite ore (δ34S is 14.7‰~24.4‰) might have been provided by the strata sulfate. 206Pb/204Pb, 207Pb/204Pb, 208Pb/204Pb ratios of 13 sulfide ore samples vary in the range of 18.627~18.942, 15.670~15.804 and 38.366~38.912, with the average value being 18.747, 15.705 and 38.614, respec?tively. These values are very similar to values of Pb isotopes of magmatic feldspar in southern Hu'nan and also have weak linear rela?tion with Pb isotopes of regional Cambrian strata, suggesting that ore materials might have mainly originated from magmatic pluton in the depth, and subordinately from the Cambrian strata. Based on the above results and geological evidence, the authors put forward a model of magma-related hydrothermal mineralization with multiple sources of ore-forming materials, which may be suitable for explaining the ore genesis of the Liushutang deposit.

关键词

铅锌矿床/成矿阶段/S同位素/Pb同位素/留书塘/湖南

Key words

lead-zinc deposit/mineral paragenesis/S isotope/Pb isotope/Liushutang/Hu'nan Province

分类

天文与地球科学

引用本文复制引用

程顺波,吴志华,刘重芃,刘阿睢,马丽艳,卢友月..湖南省留书塘铅锌矿床S、Pb同位素特征及意义[J].地质通报,2017,36(5):846-856,11.

基金项目

中国地质调查局项目《南岭成矿带中西段地质矿产调查》(编号:121201009000150002)和《右江成矿区桂西地质矿产调查》(编号:121201009000150012) (编号:121201009000150002)

地质通报

OA北大核心CSCDCSTPCD

1671-2552

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