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四川丹巴金矿床金矿物学特征及黑铋金矿的指示意义

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丹巴金矿床是位于松潘—甘孜造山带东南缘典型的碲化物型金矿床.该矿床中发育大量明金与碲铋矿物.以叶碲铋矿和自然金为主要研究对象,通过显微岩相学观察、扫描电镜能谱分析,对自然金的矿物学特征进行了较为详细的研究.结果显示,丹巴金矿床载金矿物主要有磁黄铁矿、黄铜矿、黄铁矿、叶碲铋矿、自然铋、黑铋金矿,大量自然金与叶碲铋矿、自然铋具有密切的时空关系,黑铋金矿的产出是铋熔体析出并清除金最直接的证据.
Gold mineralogical characteristics and indicative significance of maldonite in Danba Gold Deposit,Sichuan Province
Danba Gold Deposit is a typical telluride-type gold deposit located in the southeastern margin of the Songpan-Ganzi orogenic belt.A large number of visible gold and tellurium-bismuth minerals are developed in this deposit.The mineralogical characteristics of native gold were studied in detail through microscopic petrographic obser-vation and scanning electron microscopy,with pilsenite and native gold as the main research objects.The results show that the gold-bearing minerals in Danba Gold Deposit mainly include pyrrhotite,chalcopyrite,pyrite,pilsenite,native bismuth,and maldonite.A large amount of native gold has a close spatiotemporal relationship with pilsenite and native bismuth.The occurrence of maldonite is the most direct evidence of bismuth melt precipitation and gold removal.

telluride typeDanba Gold Depositmaldonitenative goldmineralogical characteristicsSongpan-Ganzi orogenic belt

马天祺、黄睿、刘效孔、陈翠华

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成都理工大学地球科学学院

四川师范大学文学院

碲化物型 丹巴金矿床 黑铋金矿 自然金 矿物学特征 松潘—甘孜造山带

四川省科技厅面上项目四川省科技厅自然科学基金项目

2018JY04772023NSFSC0274

2024

黄金
长春黄金研究院

黄金

CSTPCD
影响因子:0.446
ISSN:1001-1277
年,卷(期):2024.45(2)
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