Standard

(The distribution of elements-admixtures in the rocks and minerals of the layered dunite-troctolite-gabbronorite massif of Cavakta (south Yakutia).). / Korneev, S. I.

в: Vestnik Leningradskogo Universiteta, Geologiya-Geografiya, 1984, стр. 85-88.

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

Harvard

Korneev, SI 1984, '(The distribution of elements-admixtures in the rocks and minerals of the layered dunite-troctolite-gabbronorite massif of Cavakta (south Yakutia).)', Vestnik Leningradskogo Universiteta, Geologiya-Geografiya, стр. 85-88.

APA

Korneev, S. I. (1984). (The distribution of elements-admixtures in the rocks and minerals of the layered dunite-troctolite-gabbronorite massif of Cavakta (south Yakutia).). Vestnik Leningradskogo Universiteta, Geologiya-Geografiya, 85-88.

Vancouver

Korneev SI. (The distribution of elements-admixtures in the rocks and minerals of the layered dunite-troctolite-gabbronorite massif of Cavakta (south Yakutia).). Vestnik Leningradskogo Universiteta, Geologiya-Geografiya. 1984;85-88.

Author

Korneev, S. I. / (The distribution of elements-admixtures in the rocks and minerals of the layered dunite-troctolite-gabbronorite massif of Cavakta (south Yakutia).). в: Vestnik Leningradskogo Universiteta, Geologiya-Geografiya. 1984 ; стр. 85-88.

BibTeX

@article{d75b94226baa4047a2a9bf4eee9291d0,
title = "(The distribution of elements-admixtures in the rocks and minerals of the layered dunite-troctolite-gabbronorite massif of Cavakta (south Yakutia).)",
abstract = "There are two concordant series of rocks within this NE Siberian intrusion. Each consists of a number of differentiates ranging from dunites to titanomagnetite gabbro. The ultrabasic differentiates contain dispersed sulphides and chromitites and the upper ones, dispersed titanomagnetite. The distribution of Ni, Co, Cr, Ti and V in the rocks and mafic minerals has been analysed. It is shown that the maximum concentrations of Ti and V are typical of the upper differentiates (titanomagnetite gabbro), while mafic minerals, mainly olivines, contain a considerable concentration of Ni. -C.N.",
author = "Korneev, {S. I.}",
year = "1984",
language = "русский",
pages = "85--88",
journal = "Вестник Санкт-Петербургского университета. Науки о Земле",
issn = "1812-9323",
publisher = "Издательство Санкт-Петербургского университета",

}

RIS

TY - JOUR

T1 - (The distribution of elements-admixtures in the rocks and minerals of the layered dunite-troctolite-gabbronorite massif of Cavakta (south Yakutia).)

AU - Korneev, S. I.

PY - 1984

Y1 - 1984

N2 - There are two concordant series of rocks within this NE Siberian intrusion. Each consists of a number of differentiates ranging from dunites to titanomagnetite gabbro. The ultrabasic differentiates contain dispersed sulphides and chromitites and the upper ones, dispersed titanomagnetite. The distribution of Ni, Co, Cr, Ti and V in the rocks and mafic minerals has been analysed. It is shown that the maximum concentrations of Ti and V are typical of the upper differentiates (titanomagnetite gabbro), while mafic minerals, mainly olivines, contain a considerable concentration of Ni. -C.N.

AB - There are two concordant series of rocks within this NE Siberian intrusion. Each consists of a number of differentiates ranging from dunites to titanomagnetite gabbro. The ultrabasic differentiates contain dispersed sulphides and chromitites and the upper ones, dispersed titanomagnetite. The distribution of Ni, Co, Cr, Ti and V in the rocks and mafic minerals has been analysed. It is shown that the maximum concentrations of Ti and V are typical of the upper differentiates (titanomagnetite gabbro), while mafic minerals, mainly olivines, contain a considerable concentration of Ni. -C.N.

UR - http://www.scopus.com/inward/record.url?scp=0021556427&partnerID=8YFLogxK

M3 - статья

AN - SCOPUS:0021556427

SP - 85

EP - 88

JO - Вестник Санкт-Петербургского университета. Науки о Земле

JF - Вестник Санкт-Петербургского университета. Науки о Земле

SN - 1812-9323

ER -

ID: 94231983