| 桂西及其邻区卡林型金矿床成矿流体水源初探 |
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| 引用本文： | 解庆林,林锦富,陈余道,张学洪,王敦球.桂西及其邻区卡林型金矿床成矿流体水源初探[J].地质论评,1999,45(7):839-843. |
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| 作者姓名： | 解庆林 林锦富 陈余道 张学洪 王敦球 |
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| 作者单位： | 桂林工学院资源与环境工程系，541004 |
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| 基金项目： | 本文为国家自然科学基金（编号：49703045）及广西壮族自治区科委匹配基金联合资助。 |
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| 摘 要： | 对区内典型矿床氢氧同位素的系统研究表明：大多数矿床在大气降水参与成矿过程中具有整体性和统一性；本区矿床成矿溶液可进一步分为直接来自大气降水和主要来自沉积水两大类。
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| 关 键 词： | 卡林型金矿 水岩反应 桂西及其邻区 |
A Preliminary Study on the Water Sources of Ore forming Solutions of Carlin Type of Gold Deposits in Western Guangxi and Adjacent Regions |
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| Xie Qinglin,Lin Jingfu,Chen Yudao,Zhang Xuehong and Wang Dunqiu.A Preliminary Study on the Water Sources of Ore forming Solutions of Carlin Type of Gold Deposits in Western Guangxi and Adjacent Regions[J].Geological Review,1999,45(7):839-843. |
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| Authors: | Xie Qinglin Lin Jingfu Chen Yudao Zhang Xuehong and Wang Dunqiu |
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| Institution: | Guilin institute of Technology, Guilin, 541004 |
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| Abstract: | According to measured data of more than 50 inclusions in the ores from 12 depos i ts in western Guangxi and adjacent area, the authors complied a deuterium contou r map for the study area. It is shown that most of the ore deposits show an integrity and unity in the ore forming p r ocess of meteoric water. The deposits can be classified into two types: one with the ore forming solution originated directly from meteoric water, and another d erived mainly from sedimentary water. |
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