ОНТОГЕНИЧЕСКИЕ ОРИЕНТИРЫ ДЛЯ ВЫБОРА МОДЕЛИ ФОРМИРОВАНИЯ ПЛАТИНОВОГО ОРУДЕНЕНИЯ В ЗОНАЛЬНЫХ КЛИНОПИРОКСЕНИТ-ДУНИТОВЫХ МАССИВАХ УРАЛА

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ОНТОГЕНИЧЕСКИЕ ОРИЕНТИРЫ ДЛЯ ВЫБОРА МОДЕЛИ ФОРМИРОВАНИЯ ПЛАТИНОВОГО ОРУДЕНЕНИЯ В ЗОНАЛЬНЫХ КЛИНОПИРОКСЕНИТ-ДУНИТОВЫХ МАССИВАХ УРАЛА. / Stepanov, S. Y.; Palamarchuk, R. S.; Minibayev, A. M.

в: Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, Том 148, № 2, 01.02.2019, стр. 115-130.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

BibTeX

@article{069c748357a9421e8505d0ecda233a63,

title = "ОНТОГЕНИЧЕСКИЕ ОРИЕНТИРЫ ДЛЯ ВЫБОРА МОДЕЛИ ФОРМИРОВАНИЯ ПЛАТИНОВОГО ОРУДЕНЕНИЯ В ЗОНАЛЬНЫХ КЛИНОПИРОКСЕНИТ-ДУНИТОВЫХ МАССИВАХ УРАЛА",

abstract = "Results of ontogenetic studies of the early paragenesis of ore minerals in zonal clinopyroxenitedunite massifes of the Middle Urals are discussed. It is shown that the formation of these minerals occurs in the following order: iridosmium → chrome-spinel → laurite-erlichmanite → osmiridium → isoferroplatinum. Revealed ontogenic features of ore phases are in good agreement with models suggesting the concentration of platinum group metals at the magmatic stage of evolution of the clinopyroxenite-dunite massif before display of the superimposed high-temperature plastic deformation.",

keywords = "Chrome-spinel, Clinopyroxenite-dunite massifs, Iridium, Native platinum, Ontogenetic studies, Osmium, Paragenesis, The Middle Urals",

author = "Stepanov, {S. Y.} and Palamarchuk, {R. S.} and Minibayev, {A. M.}",

year = "2019",

month = feb,

day = "1",

doi = "10.30695/zrmo/2019.1482.08",

language = "русский",

volume = "148",

pages = "115--130",

journal = "ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА",

issn = "0869-6055",

publisher = "Издательство {"}Наука{"}",

number = "2",

}

RIS

TY - JOUR

T1 - ОНТОГЕНИЧЕСКИЕ ОРИЕНТИРЫ ДЛЯ ВЫБОРА МОДЕЛИ ФОРМИРОВАНИЯ ПЛАТИНОВОГО ОРУДЕНЕНИЯ В ЗОНАЛЬНЫХ КЛИНОПИРОКСЕНИТ-ДУНИТОВЫХ МАССИВАХ УРАЛА

AU - Stepanov, S. Y.

AU - Palamarchuk, R. S.

AU - Minibayev, A. M.

PY - 2019/2/1

Y1 - 2019/2/1

N2 - Results of ontogenetic studies of the early paragenesis of ore minerals in zonal clinopyroxenitedunite massifes of the Middle Urals are discussed. It is shown that the formation of these minerals occurs in the following order: iridosmium → chrome-spinel → laurite-erlichmanite → osmiridium → isoferroplatinum. Revealed ontogenic features of ore phases are in good agreement with models suggesting the concentration of platinum group metals at the magmatic stage of evolution of the clinopyroxenite-dunite massif before display of the superimposed high-temperature plastic deformation.

AB - Results of ontogenetic studies of the early paragenesis of ore minerals in zonal clinopyroxenitedunite massifes of the Middle Urals are discussed. It is shown that the formation of these minerals occurs in the following order: iridosmium → chrome-spinel → laurite-erlichmanite → osmiridium → isoferroplatinum. Revealed ontogenic features of ore phases are in good agreement with models suggesting the concentration of platinum group metals at the magmatic stage of evolution of the clinopyroxenite-dunite massif before display of the superimposed high-temperature plastic deformation.

KW - Chrome-spinel

KW - Clinopyroxenite-dunite massifs

KW - Iridium

KW - Native platinum

KW - Ontogenetic studies

KW - Osmium

KW - Paragenesis

KW - The Middle Urals

UR - http://www.scopus.com/inward/record.url?scp=85072344950&partnerID=8YFLogxK

UR - http://www.mendeley.com/research/ontogenetic-orientations-choose-model-formation-platinumbearing-mineralization-zonal-clinopyroxenite

U2 - 10.30695/zrmo/2019.1482.08

DO - 10.30695/zrmo/2019.1482.08

M3 - статья

AN - SCOPUS:85072344950

VL - 148

SP - 115

EP - 130

JO - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

JF - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

SN - 0869-6055

IS - 2

ER -

ID: 47659336