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Peculiarities of the chemical composition of spinel group minerals in the talnakh copper-nickel ore deposit (north-west of the Siberian platform). / Aplonov, V. S.; Zolotarev, A. A.

в: Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, Том 146, № 3, 01.01.2017, стр. 51-69.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

Harvard

Aplonov, VS & Zolotarev, AA 2017, 'Peculiarities of the chemical composition of spinel group minerals in the talnakh copper-nickel ore deposit (north-west of the Siberian platform)', Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, Том. 146, № 3, стр. 51-69.

APA

Vancouver

Author

Aplonov, V. S. ; Zolotarev, A. A. / Peculiarities of the chemical composition of spinel group minerals in the talnakh copper-nickel ore deposit (north-west of the Siberian platform). в: Zapiski Rossiiskogo Mineralogicheskogo Obshchestva. 2017 ; Том 146, № 3. стр. 51-69.

BibTeX

@article{8b654da350264235a3f6efd7334db26f,
title = "Peculiarities of the chemical composition of spinel group minerals in the talnakh copper-nickel ore deposit (north-west of the Siberian platform)",
abstract = " There are generalized data of the representative collection of chemical analyses of spinel group minerals from various rocks of the Talnakh deposit (in total - 240 microprobe analyses). Data on composition of spinelids from rocks of Zubovskoe (4 analyses) and Norilsk-1 (53 analyses) deposits have been used also. Spinel group minerals in igneous rocks and the metamorphic halo of the Talnakh deposit belong to five mineral species: magnetite, chromite, magnesiochromite, spinel and hercynite. Magnesioferrite, maghemite and titanomaghemite may be present in the ore field rocks also: some chemical analyses in the studied collection might be recalculated in chemical formulas of these mineral species. Ulvospinel was identified in rocks of Norilsk-I and Zubovskoe deposits. Despite the diversity of spinel group minerals, variations of their compositions are described by only three schemes of isomorphism: Mg ↔ Fe 2+ ; Al ↔ Fe 3+ ↔ Cr; Fe 3+VI + Fe 3+IV ↔ Ti 4+VI + Fe 2+IV . The role of other elements - Si, Ni, Co, Mn, Ca, Na, K, Zn, V - is insignificant. ",
keywords = "Chemical composition, Spinel group, Talnakh deposit",
author = "Aplonov, {V. S.} and Zolotarev, {A. A.}",
year = "2017",
month = jan,
day = "1",
language = "English",
volume = "146",
pages = "51--69",
journal = "ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА",
issn = "0869-6055",
publisher = "Издательство {"}Наука{"}",
number = "3",

}

RIS

TY - JOUR

T1 - Peculiarities of the chemical composition of spinel group minerals in the talnakh copper-nickel ore deposit (north-west of the Siberian platform)

AU - Aplonov, V. S.

AU - Zolotarev, A. A.

PY - 2017/1/1

Y1 - 2017/1/1

N2 - There are generalized data of the representative collection of chemical analyses of spinel group minerals from various rocks of the Talnakh deposit (in total - 240 microprobe analyses). Data on composition of spinelids from rocks of Zubovskoe (4 analyses) and Norilsk-1 (53 analyses) deposits have been used also. Spinel group minerals in igneous rocks and the metamorphic halo of the Talnakh deposit belong to five mineral species: magnetite, chromite, magnesiochromite, spinel and hercynite. Magnesioferrite, maghemite and titanomaghemite may be present in the ore field rocks also: some chemical analyses in the studied collection might be recalculated in chemical formulas of these mineral species. Ulvospinel was identified in rocks of Norilsk-I and Zubovskoe deposits. Despite the diversity of spinel group minerals, variations of their compositions are described by only three schemes of isomorphism: Mg ↔ Fe 2+ ; Al ↔ Fe 3+ ↔ Cr; Fe 3+VI + Fe 3+IV ↔ Ti 4+VI + Fe 2+IV . The role of other elements - Si, Ni, Co, Mn, Ca, Na, K, Zn, V - is insignificant.

AB - There are generalized data of the representative collection of chemical analyses of spinel group minerals from various rocks of the Talnakh deposit (in total - 240 microprobe analyses). Data on composition of spinelids from rocks of Zubovskoe (4 analyses) and Norilsk-1 (53 analyses) deposits have been used also. Spinel group minerals in igneous rocks and the metamorphic halo of the Talnakh deposit belong to five mineral species: magnetite, chromite, magnesiochromite, spinel and hercynite. Magnesioferrite, maghemite and titanomaghemite may be present in the ore field rocks also: some chemical analyses in the studied collection might be recalculated in chemical formulas of these mineral species. Ulvospinel was identified in rocks of Norilsk-I and Zubovskoe deposits. Despite the diversity of spinel group minerals, variations of their compositions are described by only three schemes of isomorphism: Mg ↔ Fe 2+ ; Al ↔ Fe 3+ ↔ Cr; Fe 3+VI + Fe 3+IV ↔ Ti 4+VI + Fe 2+IV . The role of other elements - Si, Ni, Co, Mn, Ca, Na, K, Zn, V - is insignificant.

KW - Chemical composition

KW - Spinel group

KW - Talnakh deposit

UR - http://www.scopus.com/inward/record.url?scp=85063747189&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:85063747189

VL - 146

SP - 51

EP - 69

JO - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

JF - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

SN - 0869-6055

IS - 3

ER -

ID: 47738584