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Kravtsovite, PdAg (sub 2) S, a new mineral from the Noril'sk-Talnakh Deposit, Krasnoyarskiy Kray, Russia

Anna Vymazalova, Frantisek Laufek, Sergei F. Sluzhenikin, Chris J. Stanley, Vladimir V. Kozlov, Dmitry A. Chareev and Maria L. Lukashova
Kravtsovite, PdAg (sub 2) S, a new mineral from the Noril'sk-Talnakh Deposit, Krasnoyarskiy Kray, Russia
European Journal of Mineralogy (June 2017) 29 (4): 597-602

Abstract

Kravtsovite, PdAg (sub 2) S, is a new platinum-group mineral discovered in the Komsomolsky mine of the Talnakh deposit, Noril'sk district, Russia. It forms equant inclusions (ranging in size from a few D:\Palash\HWNLM\07_06m to 40-50 D:\Palash\HWNLM\07_06m) in silicates and pyrite, commonly intergrown with vysotskite and Au-Ag alloy in aggregates (100-200 D:\Palash\HWNLM\07_06m across) with telargpalite, cooperite, braggite, vysotskite, sopcheite, stibiopalladinite, sobolevskite, moncheite, kotulskite, malyshevite and insizwaite. Kravtsovite is brittle; it has a metallic lustre and a grey streak. In plane-polarised light, kravtsovite is yellowish white, has strong bireflectance, is strongly pleochroic in shades of slightly yellowish white to bluish grey, and exhibits a strong anisotropy with rotation tints of salmon-pink, orange, pale blue and dark blue-black. It exhibits no internal reflections. Reflectance values in air (R (sub 1) , R (sub 2) in %) are: 32.2, 38.3 at 470, 31.6, 39.4 at 546, 30.2, 39.8 at 589 and 28.8, 41.1 at 650 nm. Eighteen electron probe microanalyses of kravtsovite give the average composition: Pd 30.53, Ag 60.11, S 8.47, and Se 0.74, total 99.85 wt%, corresponding to the empirical formula Pd (sub 1.03) Ag (sub 1.99) (S (sub 0.95) Se (sub 0.03) ) (sub Sigma 0.98) based on a total of 4 atoms per formula unit (apfu). The average of eight analyses on synthetic kravtsovite is: Pd 30.98, Ag 60.27, and S 8.81, total 100.07 wt%, corresponding to Pd (sub 1.04) Ag (sub 1.99) S (sub 0.98) . The mineral is orthorhombic, space group Cmcm, with a 7.9835(1), b 5.9265(1), c 5.7451(1) A, V 271.82(1) A (super 3) and Z = 4. The crystal structure was refined from the powder X-ray-diffraction data of the synthetic analogue. The strongest lines in the X-ray powder diffraction pattern of synthetic kravtsovite [d in A(I) (hkl)] are: 2.632(51)(021), 2.458(65)(112), 2.4263(71)(310), 2.3305(60)(202), 2.2352(100)(311), 2.1973(48) (221), 2.0619(42)(022), 1.9172(30)(130), 1.3888(31)(240,332), 1.3586(28)(512). The mineral honours V.F. Kravtsov, one of the discoverers of the Talnakh and Oktyabrsk deposits in the Noril'sk district of Russia.


ISSN: 0935-1221
EISSN: 1617-4011
Serial Title: European Journal of Mineralogy
Serial Volume: 29
Serial Issue: 4
Title: Kravtsovite, PdAg (sub 2) S, a new mineral from the Noril'sk-Talnakh Deposit, Krasnoyarskiy Kray, Russia
Affiliation: Czech Geological Survey, Czech Republic
Pages: 597-602
Published: 20170608
Text Language: English
Publisher: Schweizerbart'sche Verlagsbuchhandlung (Naegele u. Obermiller), Stuttgart, Germany
References: 14
Accession Number: 2017-082594
Categories: Mineralogy of non-silicates
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 5 tables
N69°00'00" - N69°00'00", E88°00'00" - E88°00'00"
Secondary Affiliation: Russian Academy of Sciences, Institute of Geology of Ore Deposits, Mineralogy, Petrography and Geochemistry, RUS, Russian FederationNatural History Museum, GBR, United KingdomOxford Instruments, GBR, United KingdomRussian Academy of Sciences, Institute of Experimental Mineralogy, RUS, Russian FederationTescan CIS, RUS, Russian Federation
Country of Publication: Germany
Secondary Affiliation: GeoRef, Copyright 2022, American Geosciences Institute. Abstract, copyright, Schweizerbart'sche Verlagsbuchhandlung. Reference includes data from GeoScienceWorld, Alexandria, VA, United States
Update Code: 201743
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