Unnamed Pt(Cu0.67Sn0.33) from the Bolshoy Khailyk River, Western Sayans, Russia, and a Review of Related Compounds and Solid Solutions

Barkov, Andrei Y.; Bindi, Luca; Juárez-Arellano, Erick A.; Tamura, Nobumichi; Shvedov, Gennadiy I.; Ma, Chi; Martin, Robert F.

doi:10.3390/min11111240

Title: Unnamed Pt(Cu_0.67Sn_0.33) from the Bolshoy Khailyk River, Western Sayans, Russia, and a Review of Related Compounds and Solid Solutions

Journal Article · 07 November 2021 · Minerals

DOI: https://doi.org/10.3390/min11111240 · OSTI ID:1896667

Barkov, Andrei Y. ^[1];

^[2];

^[3];

^[4];

^[5];

^[6]; Martin, Robert F. ^[7]

Cherepovets State University, Cherepovets (Russian Federation)
Univ. degli Studi di Firenze (Italy)
University of Papaloapan, Oaxaca (Mexico)
Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States). Advanced Light Source (ALS)
Siberian Federal Univ., Krasnoyarsk (Russian Federation)
California Institute of Technology (CalTech), Pasadena, CA (United States)
McGill Univ., Montreal, QC (Canada)

We describe a potentially new species of a platinum cupride–stannide mineral (PCSM) of composition Pt(Cu_0.67Sn_0.33). It occurs in a placer deposit in the River Bolshoy Khailyk, southern Krasnoyarskiy kray, Russia. A synthetic equivalent of PCSM was obtained and characterized. The PCSM occurs as anhedral or subhedral grains up to 15 μm × 30 μm in association with various platinum-group minerals, Rh–Co-rich pentlandite and magnetite, all hosted by a placer grain of Cu–Au–Pt alloy. Synchrotron micro-Laue diffraction studies indicate that the PCSM mineral is tetragonal and belongs to the inferred space-group P4/mmm (#123). Its unit-cell parameters are a = 2.838 (3) Å, c = 3.650 (4) Å, and V = 29.40 (10) Å³, and Z = 1. The c:a ratio calculated from the unit-cell parameters is 1.286. These characteristics are in good agreement with those obtained for specimens of synthetic Pt(Cu_0.67Sn_0.33). A review on related minerals and unnamed phases is provided to outline compositional variations and extents of solid solutions in the relevant systems PtNi–PtFe–PtCu, PdCu–PdHg–PdAu, PdHg–PtHg, and AuCu–PtCu. The PCSM-bearing mineralization appears to be related genetically with an ophiolitic source-rock of the Aktovrakskiy complex of the western Sayans. The unnamed phase likely crystallized from microvolumes of a highly fractionated melt rich in Cu and Sn.

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Research Organization:: Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)

Sponsoring Organization:: USDOE Office of Science (SC), Basic Energy Sciences (BES)

Grant/Contract Number:: AC02-05CH11231

OSTI ID:: 1896667

Journal Information:: Minerals, Journal Name: Minerals Journal Issue: 11 Vol. 11; ISSN 2075-163X

Publisher:: MDPICopyright Statement

Country of Publication:: United States

Language:: English

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Title: Unnamed Pt(Cu0.67Sn0.33) from the Bolshoy Khailyk River, Western Sayans, Russia, and a Review of Related Compounds and Solid Solutions

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Title: Unnamed Pt(Cu_0.67Sn_0.33) from the Bolshoy Khailyk River, Western Sayans, Russia, and a Review of Related Compounds and Solid Solutions