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陕西省岩房湾铅锌矿成矿流体与地球化学特征

刘必政 王建平 曾祥涛 王可心 曹瑞荣 程建军

地质找矿论丛2013,Vol.28Issue(1):50-57,8.
地质找矿论丛2013,Vol.28Issue(1):50-57,8.DOI:10.6053/j.issn.1001-1412.2013.01.007

陕西省岩房湾铅锌矿成矿流体与地球化学特征

Ore fluid and geochemical characteristics of Yanfangwan Pb-Zn deposit in Shaanxi Province

刘必政 1王建平 1曾祥涛 1王可心 1曹瑞荣 1程建军1

作者信息

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摘要

Abstract

Yanefangwan Pb-Zn deposit is a small Pb-Zn deposit of Fengtai ore-deposit-cluster area in Taibai county, Shaanxi Province and a few geological works have been done. Ore fluid of Yanfangwan Pb-Zn deposit is in medium-low temperature and low salinity and contains CO2, N2, CH4 etc. of the reductive gas system characteristic of hot saline. The fluid inclusions are mainly water solution, COz-H2O-NaCl and pure CO2, the three kinds of inclusion which are immisible. The homogenization temperature is higher than that of Bafangshan-Erlihe Pb-Zn deposit that may be related to intrusion of Xiba rock body. H,0 iso-topic composition is characterized by mixture of magmatic water and metamorphic water, C,O isotopic composition by normal Silurian marine carbonate rock and Pb isotopic composition by mixture of Pb sourced from orogenic belt and that of upper crust. Isotopic characteristics of Yanfangwan Pb-Zn deposit differs obviously from those of large Sedex Pb-Zn deposits in the same area and is inapropriately classified into the hot water sedimentary large Pb-Zn deposit.

关键词

岩房湾铅锌矿/流体包裹体/成矿流体/地球化学/凤太矿集区/陕西省

Key words

Yanfangwan Pb-Zn deposit/fluid inclusion/ore fluid/geochemistry/Fengtai ore-deposit-cluster area/Shaanxi Province

分类

天文与地球科学

引用本文复制引用

刘必政,王建平,曾祥涛,王可心,曹瑞荣,程建军..陕西省岩房湾铅锌矿成矿流体与地球化学特征[J].地质找矿论丛,2013,28(1):50-57,8.

基金项目

国家自然科学基金项目(编号:41030423)和中国黄金集团公司科技项目"陕西省太白县双王金矿床地质特征、成矿规律及找矿靶区再研究"联合资助. (编号:41030423)

地质找矿论丛

OACSCDCSTPCD

1001-1412

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