| 广西老厂式铅锌矿床成因研究 |
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| 引用本文： | 陆孝赞,黄位鸿,卫小彦,秦荣娥.广西老厂式铅锌矿床成因研究[J].矿产与地质,2004,18(2):139-142. |
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| 作者姓名： | 陆孝赞 黄位鸿 卫小彦 秦荣娥 |
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| 作者单位： | 广西地质勘查总院第一勘查院,广西,桂林,541100 |
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| 基金项目： | 2002年广西地质勘查专项基金项目(2002)09资助。 |
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| 摘 要： | 老厂式铅锌矿是产于泥盆系和寒武系不整合界面之间的脉状中温热液铅锌矿床，受断裂构造控制。成矿物质来源于深部岩浆和基底地层，成矿流体以岩浆水为主，混有部分雨水的混合水。矿床成因属沉积-岩浆热液改造富集矿床。
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| 关 键 词： | 铅锌矿床 成因 成矿模式 老厂式 广西 |
| 文章编号： | 1001-5663(2004)02-0139-04 |
| 修稿时间： | 2003年2月20日 |
GENESIS OF LEAD AND ZINC DEPOSIT OF LAOCHANG TYPE, GUANGXI |
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| LU Xiao-zhan,HUANG Wei-hong,WEI Xiao-yan,QIN Rong-e.GENESIS OF LEAD AND ZINC DEPOSIT OF LAOCHANG TYPE, GUANGXI[J].Mineral Resources and Geology,2004,18(2):139-142. |
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| Authors: | LU Xiao-zhan HUANG Wei-hong WEI Xiao-yan QIN Rong-e |
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| Abstract: | Lead and zinc deposit of laochang type is mesothermal deposit of vein type that occur in an unconformity interface between Devonian and Cambrian strata and controlled by fracture structure. Ore material was origin in deep magma and basement rock. Magma water is the main ore fluid mixed with some meteoric water. The genesis of the deposit belongs to transformed and accumulated deposit of deposition and magmatic hydrothermal. |
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| Keywords: | Lead and zinc deposit genesis metallogenc model Laochang type Guangxi |
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