Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Platinum group minerals from the deluvial placer of the Veresovka River, Veresovoborsky dunite-clinopyroxenite massif (the Middle Urals). / Stepanov, S. Y.; Palamarchuk, R. S.; Varlamov, D. A.; Kozlov, A. V.; Khanin, D. A.; Antonov, A. V.
в: Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, Том 147, № 5, 01.01.2018, стр. 40-60.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Platinum group minerals from the deluvial placer of the Veresovka River, Veresovoborsky dunite-clinopyroxenite massif (the Middle Urals)
AU - Stepanov, S. Y.
AU - Palamarchuk, R. S.
AU - Varlamov, D. A.
AU - Kozlov, A. V.
AU - Khanin, D. A.
AU - Antonov, A. V.
PY - 2018/1/1
Y1 - 2018/1/1
N2 - For the first time data on platinum group minerals (PGM) from the deluvial placer of the Veresovka River are given, their root source are dunites of the northern part of the Veresovoborsky massif. There have been identified, among minerals typical for this type of placers, Pt-Fe minerals, Os-Ir-(Ru) intermetallides, kashinite, bowieite, laurite, erlychmanite, and Ir-Rh thiospinels. There were revealed also, rare for platinum placers associated with the zonal clinopyroxenite-dunite massifs, but widely distributed in the studied placer: irarsite, hollingworthite, zvyagintsevite, potarite, cupperite, ferhodsite, and some unnamed Pb-Òå minerals. Xingzhongite has been detected there for the first time in placers of the Ural Platinum Belt. For all these minerals their morphological features are characterized in detail, together with their chemical composition determined by X-ray spectral analysis. Their genetic relationships are characterized taking into account total obtained data. This comprehensive study of PGM individuals and aggregates is used as the base to distinguish parageneses in their association.
AB - For the first time data on platinum group minerals (PGM) from the deluvial placer of the Veresovka River are given, their root source are dunites of the northern part of the Veresovoborsky massif. There have been identified, among minerals typical for this type of placers, Pt-Fe minerals, Os-Ir-(Ru) intermetallides, kashinite, bowieite, laurite, erlychmanite, and Ir-Rh thiospinels. There were revealed also, rare for platinum placers associated with the zonal clinopyroxenite-dunite massifs, but widely distributed in the studied placer: irarsite, hollingworthite, zvyagintsevite, potarite, cupperite, ferhodsite, and some unnamed Pb-Òå minerals. Xingzhongite has been detected there for the first time in placers of the Ural Platinum Belt. For all these minerals their morphological features are characterized in detail, together with their chemical composition determined by X-ray spectral analysis. Their genetic relationships are characterized taking into account total obtained data. This comprehensive study of PGM individuals and aggregates is used as the base to distinguish parageneses in their association.
KW - Erlichmanite
KW - Iridium
KW - Isoferroplatinum
KW - Kashinite
KW - Osmium
KW - Parageneses of minerals
KW - Platinum placers
KW - Potarite
KW - Pt-Fe minerals
KW - Tetraferroplatinum
KW - Ural platinum belt
KW - Veresovoborsky massif
KW - Xingzhongite
KW - Zvyagintsevite
UR - http://www.scopus.com/inward/record.url?scp=85063751723&partnerID=8YFLogxK
U2 - 10.30695/zrmo/2018.1475.03
DO - 10.30695/zrmo/2018.1475.03
M3 - Article
AN - SCOPUS:85063751723
VL - 147
SP - 40
EP - 60
JO - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА
JF - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА
SN - 0869-6055
IS - 5
ER -
ID: 47778983