MORPHOLOGY AND INTERNAL STRUCTURE OF PGE MINERALS FROM CHROMITITES OF ALKALINE-ULTRAMAFIC KONDYOR MASSIF (ALDAN SHIELD, RUSSIA)

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MORPHOLOGY AND INTERNAL STRUCTURE OF PGE MINERALS FROM CHROMITITES OF ALKALINE-ULTRAMAFIC KONDYOR MASSIF (ALDAN SHIELD, RUSSIA). / Temnikov, A.A.; Petrov , S.V.; S.Yu. , Stepanov .

In: MAGMATISM OF THE EARTH AND RELATED STRATEGIC METAL DEPOSITS, Vol. 36, 25.04.2019, p. 305-308.

Research output: Contribution to journal › Article

BibTeX

@article{a11baa9f171346ec83035da729471fe3,

title = "MORPHOLOGY AND INTERNAL STRUCTURE OF PGE MINERALS FROM CHROMITITES OF ALKALINE-ULTRAMAFIC KONDYOR MASSIF (ALDAN SHIELD, RUSSIA)",

abstract = "A limited occurence of metacrystals and pseudomorphs of secondary minerals, including tulameenite, tetraferroplatinum, ferronickelplatinum, makes a difference between Kondyor massif and Ural or Koryak zoned clinopyroxenite-dunite massifs of folding regions. A prevalence of tetraferroplatinum-group minerals among total amount of PGM from chromitites of Ural or Koryak zoned massifs is a result of their island arc origin, where the basic magmatism is accompanied by large amount of water fluids (Ivanov, 2011). Limited presence of secondary minerals can appear to be typomorphic sign of PGM association in chromitites from clinopyroxenite-dunite massifs formed in inner parts of platform. ",

author = "A.A. Temnikov and S.V. Petrov and Stepanov S.Yu.",

year = "2019",

month = apr,

day = "25",

language = "English",

volume = "36",

pages = "305--308",

journal = "MAGMATISM OF THE EARTH AND RELATED STRATEGIC METAL DEPOSITS",

issn = "2618-835X",

publisher = "ГЕОХИ РАН",

}

RIS

TY - JOUR

T1 - MORPHOLOGY AND INTERNAL STRUCTURE OF PGE MINERALS FROM CHROMITITES OF ALKALINE-ULTRAMAFIC KONDYOR MASSIF (ALDAN SHIELD, RUSSIA)

AU - Temnikov, A.A.

AU - Petrov , S.V.

AU - S.Yu. , Stepanov

PY - 2019/4/25

Y1 - 2019/4/25

N2 - A limited occurence of metacrystals and pseudomorphs of secondary minerals, including tulameenite, tetraferroplatinum, ferronickelplatinum, makes a difference between Kondyor massif and Ural or Koryak zoned clinopyroxenite-dunite massifs of folding regions. A prevalence of tetraferroplatinum-group minerals among total amount of PGM from chromitites of Ural or Koryak zoned massifs is a result of their island arc origin, where the basic magmatism is accompanied by large amount of water fluids (Ivanov, 2011). Limited presence of secondary minerals can appear to be typomorphic sign of PGM association in chromitites from clinopyroxenite-dunite massifs formed in inner parts of platform.

AB - A limited occurence of metacrystals and pseudomorphs of secondary minerals, including tulameenite, tetraferroplatinum, ferronickelplatinum, makes a difference between Kondyor massif and Ural or Koryak zoned clinopyroxenite-dunite massifs of folding regions. A prevalence of tetraferroplatinum-group minerals among total amount of PGM from chromitites of Ural or Koryak zoned massifs is a result of their island arc origin, where the basic magmatism is accompanied by large amount of water fluids (Ivanov, 2011). Limited presence of secondary minerals can appear to be typomorphic sign of PGM association in chromitites from clinopyroxenite-dunite massifs formed in inner parts of platform.

UR - https://www.elibrary.ru/item.asp?id=39112236

M3 - Article

VL - 36

SP - 305

EP - 308

JO - MAGMATISM OF THE EARTH AND RELATED STRATEGIC METAL DEPOSITS

JF - MAGMATISM OF THE EARTH AND RELATED STRATEGIC METAL DEPOSITS

SN - 2618-835X

ER -

ID: 62077737