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Platinum-group minerals in dolerites from Alexandra Land Island (Franz Josef Land Archipelago)

机译:亚历山德拉土地岛(弗朗兹·约瑟夫·土地群岛)白云岩中​​的铂族矿物

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摘要

Lavas in Alexandra Land Island of the Franz Josef Land Archipelago bear Au-Cu-Pd-type mineralization. The found mineral species belong to the Cu-Au-Pd and Pd-Cu-(Te + Sb + S + As) systems being, respectively, (i) cuproauride (Au(Cu, Pd)) and auricupride (Au(Cu,Pd)(3)) and (ii) phases similar to skaergaardite (PdCu), nielsenite (PdCu3), and numerous S-Te-Sb-Pd-Cu phases of various compositions. The morphology of PGM existing as tiny grains and films along the boundaries of plagioclase and clinopyroxene and in cracks, their crystallization at low temperatures predicted by experimental data, and the presence of native copper with sulfur impurity are signatures of postmagmatic origin. The Alexandra Land tholeiitic basalts and dolerites were, most likely, produced by the hotspot which may be the source of PGE-bearing intrusions in eastern Greenland that contain PGM similar to those discussed in the paper. (C) 2016, V.S. Sobolev IGM, Siberian Branch of the RAS. Published by Elsevier B.V. All rights reserved.
机译:弗朗兹·约瑟夫(Franz Josef)土地群岛的亚历山德拉(Alexandra)岛上的拉瓦斯(Lavas)拥有金-铜-钯-型矿化作用。所发现的矿物种类分别属于Cu-Au-Pd和Pd-Cu-(Te + Sb + S + As)系统,分别是(i)铜金(Au(Cu,Pd))和auricupride(Au(Cu, Pd)(3))和(ii)相类似于钙长石(PdCu),镍铁矿(PdCu3)和各种组成的S-Te-Sb-Pd-Cu相。 PGM的形态为沿斜长石和斜向辉石的边界以及裂缝中的微小晶粒和薄膜,通过实验数据预测它们在低温下的结晶,以及存在具有硫杂质的天然铜的存在是后岩浆成因的特征。亚历山德拉地带的玄武岩和白云岩极有可能是由热点产生的,而热点可能是格陵兰岛东部含PGE的侵入物的来源,其中含有与本文讨论的PGM相似的PGM。 (C)2016,V.S. Sobolev IGM,RAS的西伯利亚分公司。由Elsevier B.V.发布。保留所有权利。

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