首页> 外文期刊>Geology of Ore Deposits: A Journal of Theoretical and Applied Papers on All Aspects of Ore Genesis >Occurrence of Sn-Bearing Colusite in the Ore-Body 'T' of the Bor Copper Deposit, Serbia1
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Occurrence of Sn-Bearing Colusite in the Ore-Body 'T' of the Bor Copper Deposit, Serbia1

机译:塞尔维亚博尔铜矿床的矿体“ T”中含锡的辉石矿的赋存

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摘要

The ore body "T" is the newly discovered massive-pyrite type one which is located in the central part of the Bor copper mine. The main copper minerals are chalcocite-digenite, covellite and enargite. Small amounts of colusite are frequently present in the ore-body. It mostly occurs as the distinct exsolutions in digenite and, associating with enargite and covellite. Composition of the studied colusite shows enriched Sn content, giving an empirical formula from Cu_(24.7)V_(1.8)Fe_(0.2)Sb_(0.2)Sn_(0.8)S_(32) to Cu_(26.7)V_(2.0)Fe_(0.3)As_(3.0)Sb_(0.3)Sn_(3.5)S_(32). This colusite represents a solid solution between colusite and nekrasovite within a range of 14—54 mol % nekras-ovite. Most of the analyses show content of <50 mol % nekrasovite corresponding to the Sn-bearing colusite variety, while one analysis shows content of 54 mol % nekrasovite corresponding to the As-bearing nekrasovite.
机译:矿体“ T”是新发现的块状黄铁矿类型,位于Bor铜矿的中部。铜的主要矿物是辉绿辉石-褐铁矿,钴红岩和钠辉石。矿体中经常存在少量的堇青石。它主要以在地闪石中明显的析出物形式发生,并与硬辉石和玄武岩结合。研究的褐铁矿的组成显示出丰富的Sn含量,给出了从Cu_(24.7)V_(1.8)Fe_(0.2)Sb_(0.2)Sn_(0.8)S_(32)到Cu_(26.7)V_(2.0)Fe_( 0.3)As_(3.0)Sb_(0.3)Sn_(3.5)S_(32)。该软锰矿代表软锰矿和钠钾锰矿之间的固溶体,含量为14-54 mol%的钠钾-卵石。多数分析表明,含量小于50 mol%的钠云母对应于含Sn的辉石矿,而一项分析表明含量为54 mol%的锂云母对应于含As的钠云母。

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