| 萨瓦亚尔顿金矿床成矿物质来源的初步探讨 |
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| 引用本文： | 杨耘.萨瓦亚尔顿金矿床成矿物质来源的初步探讨[J].新疆地质,2001,19(4):271-275. |
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| 作者姓名： | 杨耘 |
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| 作者单位： | 新疆维吾尔自治区地质矿产开发勘查局第二地质大队, |
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| 摘 要： | 萨瓦亚尔顿金矿床成矿物质具有多源性。资料显示，主成矿元素金一部分来自矿区容矿地层，另一部分来自下伏地层，矿质S和C主要来自深部，特别是下伏火山岩；Pb来自于造山带。成矿溶液主要来自以大气降水为补给的地下（卤）水。
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| 关 键 词： | 南天山西段 萨瓦亚尔顿金矿床 成矿物质 成矿元素 成矿溶液来源 |
| 文章编号： | 1000-8845(2001)04-0271-05 |
| 修稿时间： | 2000年9月19日 |
PRELIMINARY STUDY OF THE SOURCE OF ORE-FORMING MINERALS OF SHAWAYAERDUN GOLD DEPOSIT |
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| YANG Yun.PRELIMINARY STUDY OF THE SOURCE OF ORE-FORMING MINERALS OF SHAWAYAERDUN GOLD DEPOSIT[J].Xinjiang Geology,2001,19(4):271-275. |
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| Authors: | YANG Yun |
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| Abstract: | In the Shawayaerdun gold deposit of southwestern Tianshan, mineralizing material come from multiple source. According to study metallogenetic material, Au came from producing formation and underlying stratum, S-C from the depth underlaing volcanic zone and Pb from the orogenic zone. Mineralizing solution origined from underground hydrothermal brine water. They compensating from the precipitate water, meaning can not exclude the metamorphic water and magmatic water participation. |
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| Keywords: | the southwestern Tianshan gold deposit of Shawayaerdun mineralizing element mineralizing solution mineralizing material source |
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