| 新疆阿克希克金矿地球化学异常的研究 |
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| 引用本文： | 吴礼道,周维康,王占宇. 新疆阿克希克金矿地球化学异常的研究[J]. 地质找矿论丛, 1993, 8(1): 73-83 |
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| 作者姓名： | 吴礼道 周维康 王占宇 |
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| 作者单位： | 南京地质矿产研究所(吴礼道，周维康)，南京地质矿产研究所(王占宇) |
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| 基金项目： | 本文系七五”国家重点攻关项目(75～56项)下设的《新疆阿尔泰东段金矿靶区优选和快速迫踪评价》(75～56l-I8-9)专题)的部分研究成果 |
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| 摘 要： |
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| 关 键 词： | 金矿床 地球化学 矿床地质 |
A STUDY ON GEOCHEMICAL ANOMALIES OF AKEXIKE GOLD DEPOSIT |
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| Wu Lidao,Zhou Weikang and Wang Zhanyu. A STUDY ON GEOCHEMICAL ANOMALIES OF AKEXIKE GOLD DEPOSIT[J]. Contributions to Geology and Mineral Resources Research, 1993, 8(1): 73-83 |
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| Authors: | Wu Lidao Zhou Weikang Wang Zhanyu |
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| Affiliation: | IGMR, Nanjing;IGMR, Nanjing;IGMR, Nanjing |
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| Abstract: | Akexike gold deposit is situated in eastern Altai, Xinjiang. It is a meso-epithermal vein type gold deposit which occurs in intermediate-mafic volcanic rocks. The characteristics of the geochemical anomalies of the deposit have been described in this paper. Study on geochemical data of the deposit indicates that the element association of gold mineralization is Au-As-Bi-Ag, and that the primary anomaly of gold element is directly caused by gold ore bodies. Thus, the primary gold anomaly is a direct mark in discovering gold mineralization. According to comparing between the primary and the secondery anomalies, it is obvious that both of the anomalies are of the same significance in discovering gold mineralization. |
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