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论云南会泽富铅锌矿床成矿模式
引用本文:韩润生,刘丛强,黄智龙,陈进,马德云,李元.论云南会泽富铅锌矿床成矿模式[J].矿物学报,2001,21(4):674-680.
作者姓名:韩润生  刘丛强  黄智龙  陈进  马德云  李元
作者单位:1. 中国科学院,地球化学研究所,
2. 云南会泽铅锌矿,
3. 昆明理工大学,
基金项目:云南省省院省校合作项目 ( 2 0 0 0YK 0 4),科学技术部攀 登计划预选项目 ( 95 预 39),云南省中青年学术和技术带头人培 养经费 ( 1999 0 0 6 ),会泽铅锌矿项目 ( 1999 1)
摘    要:通过构造地质学、矿床学、地球化学研究,认为燕山早期环太平洋板块的俯冲碰撞与小江深断裂带、曲靖-昭通隐伏断裂带的左行走滑运动为深源流体的形成和贯入提供了有利的构造背景,成矿物质主要来源于深源流体和蒸发岩层,矿体本身是富含铅锌锗等的成矿流体沿构造贯入的产物,矿床定位直接受北东构造带控制。在此基础上,提出“深源流体贯入-蒸发岩层萃取-构造控制”的成矿模式。

关 键 词:铅锌矿床  成矿模式  构造贯入成矿  云南  物质来源  地球化学
文章编号:1000-4734(2001)04-0674-07
修稿时间:2001年9月22日

GENESIS MODELING OF HUIZE LEAD-ZINC ORE DEPOSIT IN YUNNAN
Han Runsheng , Liu Congqiang Huang Zhilong Chen Jin Ma Deyun , Li Yuan.GENESIS MODELING OF HUIZE LEAD-ZINC ORE DEPOSIT IN YUNNAN[J].Acta Mineralogica Sinica,2001,21(4):674-680.
Authors:Han Runsheng  Liu Congqiang Huang Zhilong Chen Jin Ma Deyun  Li Yuan
Institution:Han Runsheng 1,2 Liu Congqiang 1 Huang Zhilong 1 Chen Jin 3 Ma Deyun 1,2 Li Yuan 2
Abstract:According to the tectonics, ore genesis and geochemistry, it is thought that a beneficial tectonic background has been provided for the formation and passing through of ore forming fluid in deep fountainhead because of the movement of annular Pacific plate and left hand movement of the Xiaojiang deep fault zone and Qujing Zhaotong concealed fault zone. Major ore forming materials originated from ore forming fluid in the deep fountainhead and vaporizing rocks. Orebodies came from the fluid in which Zn, Pb, Ge, etc. are rich. The orientation of orebodies has been controlled strictly by the fault zones of NE direction. The metallogenic model which is based on "passing through of ore forming fluid in deep fountainhead extraction of vaporizing rocks controlling of structure", has put forward.
Keywords:metallogenic model  ore  forming processes of passing  through structrue  source of ore  forming materials  Huize lead  zinc deposit  Yunnan
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