Exsolution in the Au–Au3Cu Region and Correction of the Au–Ag–Cu Phase Diagram

IF 0.7 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Geochemistry International Pub Date : 2024-12-26 DOI:10.1134/S0016702924700642
S. A. Onishchenko, K. G. Parkhacheva, Yu. V. Glukhov, S. K. Kuznetsov, N. Yu. Nikulova, E. M. Tropnikov
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Abstract

The phase composition of native gold was examined in an insufficiently studied part of the Au–Ag–Cu system in the range between pure gold and Au3Cu. In this region, a miscibility gap has been established for the Au–Ag–Cu solid solution, which is decomposed into Au–Ag–Cu and Au3Cu phases. These results in combinations with previously obtained and literature data made it possible to construct a complete phase diagram of the Au–Ag–Cu system in the gold-rich region for low (about 100°C) temperature. The diagram demonstrates the field of a homogeneous Au–Ag–Cu solid solution, and two-phase fields (Au3Cu and Au–Ag–Cu solid solution) and (AuCu and Au–Ag–Cu solid solution), which are separated by a three-phase field (Au3Cu, AuCu, and Au–Ag–Cu solid solution).

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Au-Au3Cu区域的溶出及Au-Ag-Cu相图的修正
在纯金和Au3Cu之间的Au-Ag-Cu体系中,研究了原生金的相组成。在该区域,Au-Ag-Cu固溶体形成了一个混相间隙,分解为Au-Ag-Cu和Au3Cu相。这些结果与先前获得的数据和文献数据相结合,使得在低(约100°C)温度下构建富金区Au-Ag-Cu体系的完整相图成为可能。该图展示了均匀的Au-Ag-Cu固溶体场,以及由三相场(Au3Cu、AuCu和Au-Ag-Cu固溶体)分隔的两相场(Au3Cu和Au-Ag-Cu固溶体)和(AuCu和Au-Ag-Cu固溶体)。
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来源期刊
Geochemistry International
Geochemistry International 地学-地球化学与地球物理
CiteScore
1.60
自引率
12.50%
发文量
89
审稿时长
1 months
期刊介绍: Geochemistry International is a peer reviewed journal that publishes articles on cosmochemistry; geochemistry of magmatic, metamorphic, hydrothermal, and sedimentary processes; isotope geochemistry; organic geochemistry; applied geochemistry; and chemistry of the environment. Geochemistry International provides readers with a unique opportunity to refine their understanding of the geology of the vast territory of the Eurasian continent. The journal welcomes manuscripts from all countries in the English or Russian language.
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