Platinoan Vysotskite with Inverse Zoning and Skeletal Cooperite in Metamorphosed Sulfide Ores Within the Eastern Flank of the Oktyabrskoe Deposit, Noril’sk ore Field

Abstract Platinoan vysotskite metacrystals with inverse zoning are described. Their size is up to 0.5 mm. Association of these metacrystals are characterized by a “paracrystalline microboudinage” texture—specifically, corroded vysotskite fragments of the first ($ Pd_{0.51} %$ Pt_{0.27} %$ Ni_{0.20}...
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Autor*in:	Spiridonov, E. M. [verfasserIn] Belyakov, S. N. Ivanova, Yu. A. Egorov, K. V. Naumov, D. I.

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2021

Anmerkung:	© Pleiades Publishing, Ltd. 2021. ISSN 1075-7015, Geology of Ore Deposits, 2021, Vol. 63, No. 8, pp. 842–849. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2020, published in Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, 2020, No. 6, pp. 20–31.

Übergeordnetes Werk:	Enthalten in: Geology of ore deposits - Berlin : Springer Science + Business Media B.V., 2006, 63(2021), 8 vom: Dez., Seite 842-849
Übergeordnetes Werk:	volume:63 ; year:2021 ; number:8 ; month:12 ; pages:842-849

Links:	Volltext

DOI / URN:	10.1134/S1075701521080109

Katalog-ID:	SPR050502751

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100	1		\|a Spiridonov, E. M. \|e verfasserin \|4 aut
245	1	0	\|a Platinoan Vysotskite with Inverse Zoning and Skeletal Cooperite in Metamorphosed Sulfide Ores Within the Eastern Flank of the Oktyabrskoe Deposit, Noril’sk ore Field
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500			\|a © Pleiades Publishing, Ltd. 2021. ISSN 1075-7015, Geology of Ore Deposits, 2021, Vol. 63, No. 8, pp. 842–849. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2020, published in Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, 2020, No. 6, pp. 20–31.
520			\|a Abstract Platinoan vysotskite metacrystals with inverse zoning are described. Their size is up to 0.5 mm. Association of these metacrystals are characterized by a “paracrystalline microboudinage” texture—specifically, corroded vysotskite fragments of the first ($ Pd_{0.51} %$ Pt_{0.27} %$ Ni_{0.20} %$ Fe_{0.02} $)S and second ($ Pd_{0.49} %$ Pt_{0.30} %$ Ni_{0.18} %$ Fe_{0.03} $)S generations, square vysotskite microcrystals of the third generation ($ Pd_{0.47} %$ Pt_{0.32} %$ Ni_{0.19} %$ Fe_{0.02} $)S overgrown with fourth-generation vysotskite ($ Pd_{0.45} %$ Pt_{0.33} %$ Ni_{0.19–0.21} %$ Fe_{0.01} $)S; these generations are overgrown with fifth-generation vysotskite ($ Pd_{0.45} %$ Pt_{0.35} %$ Ni_{0.18} %$ Fe_{0.02} $)S with rims of sixth-generation vysotskite ($ Pd_{0.43} %$ Pt_{0.37–0.38} %$ Ni_{0.16–0.17} %$ Fe_{0.02} $)S and the highest-Pt vysotskite of the seventh generation ($ Pd_{0.44} %$ Pt_{0.43} %$ Ni_{0.09} %$ Fe_{0.02} %$ Ru_{0.01} $)S. Platinoan vysotskite metacrystals are surrounded by halo of small skeletal microcrystals cooperite ($ Pt_{0.96–0.97} %$ Ni_{0–0.03} %$ Ru_{0.01} $)S. Platinoan vysotskite and cooperite develop in low-grade metamorphosed Co–Ni–Cu sulfide ores of the Oktyabrskoe deposit within the Noril’sk ore field, where these minerals replaced ferrous chlorite and corrensite, hydrogrossular, chalcopyrite, pentlandite, cubanite, and fassaite.
700	1		\|a Belyakov, S. N. \|4 aut
700	1		\|a Ivanova, Yu. A. \|4 aut
700	1		\|a Egorov, K. V. \|4 aut
700	1		\|a Naumov, D. I. \|4 aut
773	0	8	\|i Enthalten in \|t Geology of ore deposits \|d Berlin : Springer Science + Business Media B.V., 2006 \|g 63(2021), 8 vom: Dez., Seite 842-849 \|w (DE-627)510462294 \|w (DE-600)2230159-8 \|x 1555-6476 \|7 nnns
773	1	8	\|g volume:63 \|g year:2021 \|g number:8 \|g month:12 \|g pages:842-849
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912			\|a GBV_ILN_105
912			\|a GBV_ILN_110
912			\|a GBV_ILN_120
912			\|a GBV_ILN_138
912			\|a GBV_ILN_150
912			\|a GBV_ILN_151
912			\|a GBV_ILN_152
912			\|a GBV_ILN_161
912			\|a GBV_ILN_170
912			\|a GBV_ILN_171
912			\|a GBV_ILN_187
912			\|a GBV_ILN_213
912			\|a GBV_ILN_224
912			\|a GBV_ILN_230
912			\|a GBV_ILN_250
912			\|a GBV_ILN_281
912			\|a GBV_ILN_285
912			\|a GBV_ILN_293
912			\|a GBV_ILN_370
912			\|a GBV_ILN_602
912			\|a GBV_ILN_636
912			\|a GBV_ILN_702
912			\|a GBV_ILN_2001
912			\|a GBV_ILN_2003
912			\|a GBV_ILN_2004
912			\|a GBV_ILN_2005
912			\|a GBV_ILN_2006
912			\|a GBV_ILN_2007
912			\|a GBV_ILN_2008
912			\|a GBV_ILN_2009
912			\|a GBV_ILN_2010
912			\|a GBV_ILN_2011
912			\|a GBV_ILN_2014
912			\|a GBV_ILN_2015
912			\|a GBV_ILN_2020
912			\|a GBV_ILN_2021
912			\|a GBV_ILN_2025
912			\|a GBV_ILN_2026
912			\|a GBV_ILN_2027
912			\|a GBV_ILN_2031
912			\|a GBV_ILN_2034
912			\|a GBV_ILN_2037
912			\|a GBV_ILN_2038
912			\|a GBV_ILN_2039
912			\|a GBV_ILN_2044
912			\|a GBV_ILN_2048
912			\|a GBV_ILN_2049
912			\|a GBV_ILN_2050
912			\|a GBV_ILN_2055
912			\|a GBV_ILN_2056
912			\|a GBV_ILN_2057
912			\|a GBV_ILN_2059
912			\|a GBV_ILN_2061
912			\|a GBV_ILN_2064
912			\|a GBV_ILN_2065
912			\|a GBV_ILN_2068
912			\|a GBV_ILN_2088
912			\|a GBV_ILN_2093
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912			\|a GBV_ILN_2107
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912			\|a GBV_ILN_4249
912			\|a GBV_ILN_4251
912			\|a GBV_ILN_4305
912			\|a GBV_ILN_4306
912			\|a GBV_ILN_4307
912			\|a GBV_ILN_4313
912			\|a GBV_ILN_4322
912			\|a GBV_ILN_4323
912			\|a GBV_ILN_4324
912			\|a GBV_ILN_4325
912			\|a GBV_ILN_4326
912			\|a GBV_ILN_4328
912			\|a GBV_ILN_4333
912			\|a GBV_ILN_4334
912			\|a GBV_ILN_4335
912			\|a GBV_ILN_4336
912			\|a GBV_ILN_4338
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951			\|a AR
952			\|d 63 \|j 2021 \|e 8 \|c 12 \|h 842-849

Indexfelder

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allfields	10.1134/S1075701521080109 doi (DE-627)SPR050502751 (SPR)S1075701521080109-e DE-627 ger DE-627 rakwb eng Spiridonov, E. M. verfasserin aut Platinoan Vysotskite with Inverse Zoning and Skeletal Cooperite in Metamorphosed Sulfide Ores Within the Eastern Flank of the Oktyabrskoe Deposit, Noril’sk ore Field 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2021. ISSN 1075-7015, Geology of Ore Deposits, 2021, Vol. 63, No. 8, pp. 842–849. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2020, published in Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, 2020, No. 6, pp. 20–31. Abstract Platinoan vysotskite metacrystals with inverse zoning are described. Their size is up to 0.5 mm. Association of these metacrystals are characterized by a “paracrystalline microboudinage” texture—specifically, corroded vysotskite fragments of the first ($ Pd_{0.51} %$ Pt_{0.27} %$ Ni_{0.20} %$ Fe_{0.02} $)S and second ($ Pd_{0.49} %$ Pt_{0.30} %$ Ni_{0.18} %$ Fe_{0.03} $)S generations, square vysotskite microcrystals of the third generation ($ Pd_{0.47} %$ Pt_{0.32} %$ Ni_{0.19} %$ Fe_{0.02} $)S overgrown with fourth-generation vysotskite ($ Pd_{0.45} %$ Pt_{0.33} %$ Ni_{0.19–0.21} %$ Fe_{0.01} $)S; these generations are overgrown with fifth-generation vysotskite ($ Pd_{0.45} %$ Pt_{0.35} %$ Ni_{0.18} %$ Fe_{0.02} $)S with rims of sixth-generation vysotskite ($ Pd_{0.43} %$ Pt_{0.37–0.38} %$ Ni_{0.16–0.17} %$ Fe_{0.02} $)S and the highest-Pt vysotskite of the seventh generation ($ Pd_{0.44} %$ Pt_{0.43} %$ Ni_{0.09} %$ Fe_{0.02} %$ Ru_{0.01} $)S. Platinoan vysotskite metacrystals are surrounded by halo of small skeletal microcrystals cooperite ($ Pt_{0.96–0.97} %$ Ni_{0–0.03} %$ Ru_{0.01} $)S. Platinoan vysotskite and cooperite develop in low-grade metamorphosed Co–Ni–Cu sulfide ores of the Oktyabrskoe deposit within the Noril’sk ore field, where these minerals replaced ferrous chlorite and corrensite, hydrogrossular, chalcopyrite, pentlandite, cubanite, and fassaite. Belyakov, S. N. aut Ivanova, Yu. A. aut Egorov, K. V. aut Naumov, D. I. aut Enthalten in Geology of ore deposits Berlin : Springer Science + Business Media B.V., 2006 63(2021), 8 vom: Dez., Seite 842-849 (DE-627)510462294 (DE-600)2230159-8 1555-6476 nnns volume:63 year:2021 number:8 month:12 pages:842-849 https://dx.doi.org/10.1134/S1075701521080109 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 63 2021 8 12 842-849
spelling	10.1134/S1075701521080109 doi (DE-627)SPR050502751 (SPR)S1075701521080109-e DE-627 ger DE-627 rakwb eng Spiridonov, E. M. verfasserin aut Platinoan Vysotskite with Inverse Zoning and Skeletal Cooperite in Metamorphosed Sulfide Ores Within the Eastern Flank of the Oktyabrskoe Deposit, Noril’sk ore Field 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2021. ISSN 1075-7015, Geology of Ore Deposits, 2021, Vol. 63, No. 8, pp. 842–849. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2020, published in Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, 2020, No. 6, pp. 20–31. Abstract Platinoan vysotskite metacrystals with inverse zoning are described. Their size is up to 0.5 mm. Association of these metacrystals are characterized by a “paracrystalline microboudinage” texture—specifically, corroded vysotskite fragments of the first ($ Pd_{0.51} %$ Pt_{0.27} %$ Ni_{0.20} %$ Fe_{0.02} $)S and second ($ Pd_{0.49} %$ Pt_{0.30} %$ Ni_{0.18} %$ Fe_{0.03} $)S generations, square vysotskite microcrystals of the third generation ($ Pd_{0.47} %$ Pt_{0.32} %$ Ni_{0.19} %$ Fe_{0.02} $)S overgrown with fourth-generation vysotskite ($ Pd_{0.45} %$ Pt_{0.33} %$ Ni_{0.19–0.21} %$ Fe_{0.01} $)S; these generations are overgrown with fifth-generation vysotskite ($ Pd_{0.45} %$ Pt_{0.35} %$ Ni_{0.18} %$ Fe_{0.02} $)S with rims of sixth-generation vysotskite ($ Pd_{0.43} %$ Pt_{0.37–0.38} %$ Ni_{0.16–0.17} %$ Fe_{0.02} $)S and the highest-Pt vysotskite of the seventh generation ($ Pd_{0.44} %$ Pt_{0.43} %$ Ni_{0.09} %$ Fe_{0.02} %$ Ru_{0.01} $)S. Platinoan vysotskite metacrystals are surrounded by halo of small skeletal microcrystals cooperite ($ Pt_{0.96–0.97} %$ Ni_{0–0.03} %$ Ru_{0.01} $)S. Platinoan vysotskite and cooperite develop in low-grade metamorphosed Co–Ni–Cu sulfide ores of the Oktyabrskoe deposit within the Noril’sk ore field, where these minerals replaced ferrous chlorite and corrensite, hydrogrossular, chalcopyrite, pentlandite, cubanite, and fassaite. Belyakov, S. N. aut Ivanova, Yu. A. aut Egorov, K. V. aut Naumov, D. I. aut Enthalten in Geology of ore deposits Berlin : Springer Science + Business Media B.V., 2006 63(2021), 8 vom: Dez., Seite 842-849 (DE-627)510462294 (DE-600)2230159-8 1555-6476 nnns volume:63 year:2021 number:8 month:12 pages:842-849 https://dx.doi.org/10.1134/S1075701521080109 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 63 2021 8 12 842-849
allfields_unstemmed	10.1134/S1075701521080109 doi (DE-627)SPR050502751 (SPR)S1075701521080109-e DE-627 ger DE-627 rakwb eng Spiridonov, E. M. verfasserin aut Platinoan Vysotskite with Inverse Zoning and Skeletal Cooperite in Metamorphosed Sulfide Ores Within the Eastern Flank of the Oktyabrskoe Deposit, Noril’sk ore Field 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2021. ISSN 1075-7015, Geology of Ore Deposits, 2021, Vol. 63, No. 8, pp. 842–849. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2020, published in Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, 2020, No. 6, pp. 20–31. Abstract Platinoan vysotskite metacrystals with inverse zoning are described. Their size is up to 0.5 mm. Association of these metacrystals are characterized by a “paracrystalline microboudinage” texture—specifically, corroded vysotskite fragments of the first ($ Pd_{0.51} %$ Pt_{0.27} %$ Ni_{0.20} %$ Fe_{0.02} $)S and second ($ Pd_{0.49} %$ Pt_{0.30} %$ Ni_{0.18} %$ Fe_{0.03} $)S generations, square vysotskite microcrystals of the third generation ($ Pd_{0.47} %$ Pt_{0.32} %$ Ni_{0.19} %$ Fe_{0.02} $)S overgrown with fourth-generation vysotskite ($ Pd_{0.45} %$ Pt_{0.33} %$ Ni_{0.19–0.21} %$ Fe_{0.01} $)S; these generations are overgrown with fifth-generation vysotskite ($ Pd_{0.45} %$ Pt_{0.35} %$ Ni_{0.18} %$ Fe_{0.02} $)S with rims of sixth-generation vysotskite ($ Pd_{0.43} %$ Pt_{0.37–0.38} %$ Ni_{0.16–0.17} %$ Fe_{0.02} $)S and the highest-Pt vysotskite of the seventh generation ($ Pd_{0.44} %$ Pt_{0.43} %$ Ni_{0.09} %$ Fe_{0.02} %$ Ru_{0.01} $)S. Platinoan vysotskite metacrystals are surrounded by halo of small skeletal microcrystals cooperite ($ Pt_{0.96–0.97} %$ Ni_{0–0.03} %$ Ru_{0.01} $)S. Platinoan vysotskite and cooperite develop in low-grade metamorphosed Co–Ni–Cu sulfide ores of the Oktyabrskoe deposit within the Noril’sk ore field, where these minerals replaced ferrous chlorite and corrensite, hydrogrossular, chalcopyrite, pentlandite, cubanite, and fassaite. Belyakov, S. N. aut Ivanova, Yu. A. aut Egorov, K. V. aut Naumov, D. I. aut Enthalten in Geology of ore deposits Berlin : Springer Science + Business Media B.V., 2006 63(2021), 8 vom: Dez., Seite 842-849 (DE-627)510462294 (DE-600)2230159-8 1555-6476 nnns volume:63 year:2021 number:8 month:12 pages:842-849 https://dx.doi.org/10.1134/S1075701521080109 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 63 2021 8 12 842-849
allfieldsGer	10.1134/S1075701521080109 doi (DE-627)SPR050502751 (SPR)S1075701521080109-e DE-627 ger DE-627 rakwb eng Spiridonov, E. M. verfasserin aut Platinoan Vysotskite with Inverse Zoning and Skeletal Cooperite in Metamorphosed Sulfide Ores Within the Eastern Flank of the Oktyabrskoe Deposit, Noril’sk ore Field 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2021. ISSN 1075-7015, Geology of Ore Deposits, 2021, Vol. 63, No. 8, pp. 842–849. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2020, published in Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, 2020, No. 6, pp. 20–31. Abstract Platinoan vysotskite metacrystals with inverse zoning are described. Their size is up to 0.5 mm. Association of these metacrystals are characterized by a “paracrystalline microboudinage” texture—specifically, corroded vysotskite fragments of the first ($ Pd_{0.51} %$ Pt_{0.27} %$ Ni_{0.20} %$ Fe_{0.02} $)S and second ($ Pd_{0.49} %$ Pt_{0.30} %$ Ni_{0.18} %$ Fe_{0.03} $)S generations, square vysotskite microcrystals of the third generation ($ Pd_{0.47} %$ Pt_{0.32} %$ Ni_{0.19} %$ Fe_{0.02} $)S overgrown with fourth-generation vysotskite ($ Pd_{0.45} %$ Pt_{0.33} %$ Ni_{0.19–0.21} %$ Fe_{0.01} $)S; these generations are overgrown with fifth-generation vysotskite ($ Pd_{0.45} %$ Pt_{0.35} %$ Ni_{0.18} %$ Fe_{0.02} $)S with rims of sixth-generation vysotskite ($ Pd_{0.43} %$ Pt_{0.37–0.38} %$ Ni_{0.16–0.17} %$ Fe_{0.02} $)S and the highest-Pt vysotskite of the seventh generation ($ Pd_{0.44} %$ Pt_{0.43} %$ Ni_{0.09} %$ Fe_{0.02} %$ Ru_{0.01} $)S. Platinoan vysotskite metacrystals are surrounded by halo of small skeletal microcrystals cooperite ($ Pt_{0.96–0.97} %$ Ni_{0–0.03} %$ Ru_{0.01} $)S. Platinoan vysotskite and cooperite develop in low-grade metamorphosed Co–Ni–Cu sulfide ores of the Oktyabrskoe deposit within the Noril’sk ore field, where these minerals replaced ferrous chlorite and corrensite, hydrogrossular, chalcopyrite, pentlandite, cubanite, and fassaite. Belyakov, S. N. aut Ivanova, Yu. A. aut Egorov, K. V. aut Naumov, D. I. aut Enthalten in Geology of ore deposits Berlin : Springer Science + Business Media B.V., 2006 63(2021), 8 vom: Dez., Seite 842-849 (DE-627)510462294 (DE-600)2230159-8 1555-6476 nnns volume:63 year:2021 number:8 month:12 pages:842-849 https://dx.doi.org/10.1134/S1075701521080109 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 63 2021 8 12 842-849
allfieldsSound	10.1134/S1075701521080109 doi (DE-627)SPR050502751 (SPR)S1075701521080109-e DE-627 ger DE-627 rakwb eng Spiridonov, E. M. verfasserin aut Platinoan Vysotskite with Inverse Zoning and Skeletal Cooperite in Metamorphosed Sulfide Ores Within the Eastern Flank of the Oktyabrskoe Deposit, Noril’sk ore Field 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2021. ISSN 1075-7015, Geology of Ore Deposits, 2021, Vol. 63, No. 8, pp. 842–849. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2020, published in Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, 2020, No. 6, pp. 20–31. Abstract Platinoan vysotskite metacrystals with inverse zoning are described. Their size is up to 0.5 mm. Association of these metacrystals are characterized by a “paracrystalline microboudinage” texture—specifically, corroded vysotskite fragments of the first ($ Pd_{0.51} %$ Pt_{0.27} %$ Ni_{0.20} %$ Fe_{0.02} $)S and second ($ Pd_{0.49} %$ Pt_{0.30} %$ Ni_{0.18} %$ Fe_{0.03} $)S generations, square vysotskite microcrystals of the third generation ($ Pd_{0.47} %$ Pt_{0.32} %$ Ni_{0.19} %$ Fe_{0.02} $)S overgrown with fourth-generation vysotskite ($ Pd_{0.45} %$ Pt_{0.33} %$ Ni_{0.19–0.21} %$ Fe_{0.01} $)S; these generations are overgrown with fifth-generation vysotskite ($ Pd_{0.45} %$ Pt_{0.35} %$ Ni_{0.18} %$ Fe_{0.02} $)S with rims of sixth-generation vysotskite ($ Pd_{0.43} %$ Pt_{0.37–0.38} %$ Ni_{0.16–0.17} %$ Fe_{0.02} $)S and the highest-Pt vysotskite of the seventh generation ($ Pd_{0.44} %$ Pt_{0.43} %$ Ni_{0.09} %$ Fe_{0.02} %$ Ru_{0.01} $)S. Platinoan vysotskite metacrystals are surrounded by halo of small skeletal microcrystals cooperite ($ Pt_{0.96–0.97} %$ Ni_{0–0.03} %$ Ru_{0.01} $)S. Platinoan vysotskite and cooperite develop in low-grade metamorphosed Co–Ni–Cu sulfide ores of the Oktyabrskoe deposit within the Noril’sk ore field, where these minerals replaced ferrous chlorite and corrensite, hydrogrossular, chalcopyrite, pentlandite, cubanite, and fassaite. Belyakov, S. N. aut Ivanova, Yu. A. aut Egorov, K. V. aut Naumov, D. I. aut Enthalten in Geology of ore deposits Berlin : Springer Science + Business Media B.V., 2006 63(2021), 8 vom: Dez., Seite 842-849 (DE-627)510462294 (DE-600)2230159-8 1555-6476 nnns volume:63 year:2021 number:8 month:12 pages:842-849 https://dx.doi.org/10.1134/S1075701521080109 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 63 2021 8 12 842-849
language	English
source	Enthalten in Geology of ore deposits 63(2021), 8 vom: Dez., Seite 842-849 volume:63 year:2021 number:8 month:12 pages:842-849
sourceStr	Enthalten in Geology of ore deposits 63(2021), 8 vom: Dez., Seite 842-849 volume:63 year:2021 number:8 month:12 pages:842-849
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container_title	Geology of ore deposits
authorswithroles_txt_mv	Spiridonov, E. M. @@aut@@ Belyakov, S. N. @@aut@@ Ivanova, Yu. A. @@aut@@ Egorov, K. V. @@aut@@ Naumov, D. I. @@aut@@
publishDateDaySort_date	2021-12-01T00:00:00Z
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ISSN 1075-7015, Geology of Ore Deposits, 2021, Vol. 63, No. 8, pp. 842–849. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2020, published in Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, 2020, No. 6, pp. 20–31.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Platinoan vysotskite metacrystals with inverse zoning are described. Their size is up to 0.5 mm. 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author	Spiridonov, E. M.
spellingShingle	Spiridonov, E. M. Platinoan Vysotskite with Inverse Zoning and Skeletal Cooperite in Metamorphosed Sulfide Ores Within the Eastern Flank of the Oktyabrskoe Deposit, Noril’sk ore Field
authorStr	Spiridonov, E. M.
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topic_title	Platinoan Vysotskite with Inverse Zoning and Skeletal Cooperite in Metamorphosed Sulfide Ores Within the Eastern Flank of the Oktyabrskoe Deposit, Noril’sk ore Field
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title	Platinoan Vysotskite with Inverse Zoning and Skeletal Cooperite in Metamorphosed Sulfide Ores Within the Eastern Flank of the Oktyabrskoe Deposit, Noril’sk ore Field
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title_full	Platinoan Vysotskite with Inverse Zoning and Skeletal Cooperite in Metamorphosed Sulfide Ores Within the Eastern Flank of the Oktyabrskoe Deposit, Noril’sk ore Field
author_sort	Spiridonov, E. M.
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author_browse	Spiridonov, E. M. Belyakov, S. N. Ivanova, Yu. A. Egorov, K. V. Naumov, D. I.
container_volume	63
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author-letter	Spiridonov, E. M.
doi_str_mv	10.1134/S1075701521080109
title_sort	platinoan vysotskite with inverse zoning and skeletal cooperite in metamorphosed sulfide ores within the eastern flank of the oktyabrskoe deposit, noril’sk ore field
title_auth	Platinoan Vysotskite with Inverse Zoning and Skeletal Cooperite in Metamorphosed Sulfide Ores Within the Eastern Flank of the Oktyabrskoe Deposit, Noril’sk ore Field
abstract	Abstract Platinoan vysotskite metacrystals with inverse zoning are described. Their size is up to 0.5 mm. Association of these metacrystals are characterized by a “paracrystalline microboudinage” texture—specifically, corroded vysotskite fragments of the first ($ Pd_{0.51} %$ Pt_{0.27} %$ Ni_{0.20} %$ Fe_{0.02} $)S and second ($ Pd_{0.49} %$ Pt_{0.30} %$ Ni_{0.18} %$ Fe_{0.03} $)S generations, square vysotskite microcrystals of the third generation ($ Pd_{0.47} %$ Pt_{0.32} %$ Ni_{0.19} %$ Fe_{0.02} $)S overgrown with fourth-generation vysotskite ($ Pd_{0.45} %$ Pt_{0.33} %$ Ni_{0.19–0.21} %$ Fe_{0.01} $)S; these generations are overgrown with fifth-generation vysotskite ($ Pd_{0.45} %$ Pt_{0.35} %$ Ni_{0.18} %$ Fe_{0.02} $)S with rims of sixth-generation vysotskite ($ Pd_{0.43} %$ Pt_{0.37–0.38} %$ Ni_{0.16–0.17} %$ Fe_{0.02} $)S and the highest-Pt vysotskite of the seventh generation ($ Pd_{0.44} %$ Pt_{0.43} %$ Ni_{0.09} %$ Fe_{0.02} %$ Ru_{0.01} $)S. Platinoan vysotskite metacrystals are surrounded by halo of small skeletal microcrystals cooperite ($ Pt_{0.96–0.97} %$ Ni_{0–0.03} %$ Ru_{0.01} $)S. Platinoan vysotskite and cooperite develop in low-grade metamorphosed Co–Ni–Cu sulfide ores of the Oktyabrskoe deposit within the Noril’sk ore field, where these minerals replaced ferrous chlorite and corrensite, hydrogrossular, chalcopyrite, pentlandite, cubanite, and fassaite. © Pleiades Publishing, Ltd. 2021. ISSN 1075-7015, Geology of Ore Deposits, 2021, Vol. 63, No. 8, pp. 842–849. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2020, published in Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, 2020, No. 6, pp. 20–31.
abstractGer	Abstract Platinoan vysotskite metacrystals with inverse zoning are described. Their size is up to 0.5 mm. Association of these metacrystals are characterized by a “paracrystalline microboudinage” texture—specifically, corroded vysotskite fragments of the first ($ Pd_{0.51} %$ Pt_{0.27} %$ Ni_{0.20} %$ Fe_{0.02} $)S and second ($ Pd_{0.49} %$ Pt_{0.30} %$ Ni_{0.18} %$ Fe_{0.03} $)S generations, square vysotskite microcrystals of the third generation ($ Pd_{0.47} %$ Pt_{0.32} %$ Ni_{0.19} %$ Fe_{0.02} $)S overgrown with fourth-generation vysotskite ($ Pd_{0.45} %$ Pt_{0.33} %$ Ni_{0.19–0.21} %$ Fe_{0.01} $)S; these generations are overgrown with fifth-generation vysotskite ($ Pd_{0.45} %$ Pt_{0.35} %$ Ni_{0.18} %$ Fe_{0.02} $)S with rims of sixth-generation vysotskite ($ Pd_{0.43} %$ Pt_{0.37–0.38} %$ Ni_{0.16–0.17} %$ Fe_{0.02} $)S and the highest-Pt vysotskite of the seventh generation ($ Pd_{0.44} %$ Pt_{0.43} %$ Ni_{0.09} %$ Fe_{0.02} %$ Ru_{0.01} $)S. Platinoan vysotskite metacrystals are surrounded by halo of small skeletal microcrystals cooperite ($ Pt_{0.96–0.97} %$ Ni_{0–0.03} %$ Ru_{0.01} $)S. Platinoan vysotskite and cooperite develop in low-grade metamorphosed Co–Ni–Cu sulfide ores of the Oktyabrskoe deposit within the Noril’sk ore field, where these minerals replaced ferrous chlorite and corrensite, hydrogrossular, chalcopyrite, pentlandite, cubanite, and fassaite. © Pleiades Publishing, Ltd. 2021. ISSN 1075-7015, Geology of Ore Deposits, 2021, Vol. 63, No. 8, pp. 842–849. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2020, published in Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, 2020, No. 6, pp. 20–31.
abstract_unstemmed	Abstract Platinoan vysotskite metacrystals with inverse zoning are described. Their size is up to 0.5 mm. Association of these metacrystals are characterized by a “paracrystalline microboudinage” texture—specifically, corroded vysotskite fragments of the first ($ Pd_{0.51} %$ Pt_{0.27} %$ Ni_{0.20} %$ Fe_{0.02} $)S and second ($ Pd_{0.49} %$ Pt_{0.30} %$ Ni_{0.18} %$ Fe_{0.03} $)S generations, square vysotskite microcrystals of the third generation ($ Pd_{0.47} %$ Pt_{0.32} %$ Ni_{0.19} %$ Fe_{0.02} $)S overgrown with fourth-generation vysotskite ($ Pd_{0.45} %$ Pt_{0.33} %$ Ni_{0.19–0.21} %$ Fe_{0.01} $)S; these generations are overgrown with fifth-generation vysotskite ($ Pd_{0.45} %$ Pt_{0.35} %$ Ni_{0.18} %$ Fe_{0.02} $)S with rims of sixth-generation vysotskite ($ Pd_{0.43} %$ Pt_{0.37–0.38} %$ Ni_{0.16–0.17} %$ Fe_{0.02} $)S and the highest-Pt vysotskite of the seventh generation ($ Pd_{0.44} %$ Pt_{0.43} %$ Ni_{0.09} %$ Fe_{0.02} %$ Ru_{0.01} $)S. Platinoan vysotskite metacrystals are surrounded by halo of small skeletal microcrystals cooperite ($ Pt_{0.96–0.97} %$ Ni_{0–0.03} %$ Ru_{0.01} $)S. Platinoan vysotskite and cooperite develop in low-grade metamorphosed Co–Ni–Cu sulfide ores of the Oktyabrskoe deposit within the Noril’sk ore field, where these minerals replaced ferrous chlorite and corrensite, hydrogrossular, chalcopyrite, pentlandite, cubanite, and fassaite. © Pleiades Publishing, Ltd. 2021. ISSN 1075-7015, Geology of Ore Deposits, 2021, Vol. 63, No. 8, pp. 842–849. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2020, published in Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, 2020, No. 6, pp. 20–31.
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container_issue	8
title_short	Platinoan Vysotskite with Inverse Zoning and Skeletal Cooperite in Metamorphosed Sulfide Ores Within the Eastern Flank of the Oktyabrskoe Deposit, Noril’sk ore Field
url	https://dx.doi.org/10.1134/S1075701521080109
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author2	Belyakov, S. N. Ivanova, Yu. A. Egorov, K. V. Naumov, D. I.
author2Str	Belyakov, S. N. Ivanova, Yu. A. Egorov, K. V. Naumov, D. I.
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doi_str	10.1134/S1075701521080109
up_date	2024-07-03T15:57:27.283Z
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ISSN 1075-7015, Geology of Ore Deposits, 2021, Vol. 63, No. 8, pp. 842–849. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2020, published in Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, 2020, No. 6, pp. 20–31.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Platinoan vysotskite metacrystals with inverse zoning are described. Their size is up to 0.5 mm. 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Platinoan Vysotskite with Inverse Zoning and Skeletal Cooperite in Metamorphosed Sulfide Ores Within the Eastern Flank of the Oktyabrskoe Deposit, Noril’sk ore Field

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