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DISTRIBUTION OF FE-NI-CU SULFIDE MINERALIZATION IN THE ROCKS OF THE BURAKOVSKO-AGANOZERSKIǏ LAYERED INTRUSION. / Semenov, V.S.; Korneev, S.I.; Yakovleva, O.A.; Semenov, S.V.; Kol’tsov, A.B.; Grinevich, N.G.; Zil’bershte n, A.Kh.

в: Petrology, № 3, 2004, стр. 265-281.

Результаты исследований: Научные публикации в периодических изданиях › статья

Harvard

Semenov, VS, Korneev, SI, Yakovleva, OA, Semenov, SV, Kol’tsov, AB, Grinevich, NG & Zil’bershte n, AK 2004, 'DISTRIBUTION OF FE-NI-CU SULFIDE MINERALIZATION IN THE ROCKS OF THE BURAKOVSKO-AGANOZERSKIǏ LAYERED INTRUSION', Petrology, № 3, стр. 265-281. <http://elibrary.ru/item.asp?id=11964974>

APA

Semenov, V. S., Korneev, S. I., Yakovleva, O. A., Semenov, S. V., Kol’tsov, A. B., Grinevich, N. G., & Zil’bershte n, A. K. (2004). DISTRIBUTION OF FE-NI-CU SULFIDE MINERALIZATION IN THE ROCKS OF THE BURAKOVSKO-AGANOZERSKIǏ LAYERED INTRUSION. Petrology, (3), 265-281. http://elibrary.ru/item.asp?id=11964974

Vancouver

Semenov VS, Korneev SI, Yakovleva OA, Semenov SV, Kol’tsov AB, Grinevich NG и пр. DISTRIBUTION OF FE-NI-CU SULFIDE MINERALIZATION IN THE ROCKS OF THE BURAKOVSKO-AGANOZERSKIǏ LAYERED INTRUSION. Petrology. 2004;(3):265-281.

Author

Semenov, V.S. ; Korneev, S.I. ; Yakovleva, O.A. ; Semenov, S.V. ; Kol’tsov, A.B. ; Grinevich, N.G. ; Zil’bershte n, A.Kh. / DISTRIBUTION OF FE-NI-CU SULFIDE MINERALIZATION IN THE ROCKS OF THE BURAKOVSKO-AGANOZERSKIǏ LAYERED INTRUSION. в: Petrology. 2004 ; № 3. стр. 265-281.

BibTeX

@article{37cb66db45de445b8fbb1ef9cf54d681,
title = "DISTRIBUTION OF FE-NI-CU SULFIDE MINERALIZATION IN THE ROCKS OF THE BURAKOVSKO-AGANOZERSKIǏ LAYERED INTRUSION",
abstract = "The distribution of Fe-Ni-Cu sulfide mineral in the section of the layered complex and their characteristics were discussed. The intercalation of low- and high-sulfur sulfide assemblages in the rocks of the Aganozerskiǐ block coincided with petrographic rhythms. The formation of relatively high-grade sulfide mineralization was related to the processes of late magmatic redeposition of ore matter under conditions of extensional deformations generated at the boundaries between rocks of contrasting compositions. It was shown that the formation of sulfides in amygdaloidal segregations could be related to the postmagmatic interaction of inclusion material with the host mineral.",
author = "V.S. Semenov and S.I. Korneev and O.A. Yakovleva and S.V. Semenov and A.B. Kol{\textquoteright}tsov and N.G. Grinevich and {Zil{\textquoteright}bershte n}, A.Kh.",
year = "2004",
language = "English",
pages = "265--281",
journal = "Petrology",
issn = "0869-5911",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "3",

}

RIS

TY - JOUR

T1 - DISTRIBUTION OF FE-NI-CU SULFIDE MINERALIZATION IN THE ROCKS OF THE BURAKOVSKO-AGANOZERSKIǏ LAYERED INTRUSION

AU - Semenov, V.S.

AU - Korneev, S.I.

AU - Yakovleva, O.A.

AU - Semenov, S.V.

AU - Kol’tsov, A.B.

AU - Grinevich, N.G.

AU - Zil’bershte n, A.Kh.

PY - 2004

Y1 - 2004

N2 - The distribution of Fe-Ni-Cu sulfide mineral in the section of the layered complex and their characteristics were discussed. The intercalation of low- and high-sulfur sulfide assemblages in the rocks of the Aganozerskiǐ block coincided with petrographic rhythms. The formation of relatively high-grade sulfide mineralization was related to the processes of late magmatic redeposition of ore matter under conditions of extensional deformations generated at the boundaries between rocks of contrasting compositions. It was shown that the formation of sulfides in amygdaloidal segregations could be related to the postmagmatic interaction of inclusion material with the host mineral.

AB - The distribution of Fe-Ni-Cu sulfide mineral in the section of the layered complex and their characteristics were discussed. The intercalation of low- and high-sulfur sulfide assemblages in the rocks of the Aganozerskiǐ block coincided with petrographic rhythms. The formation of relatively high-grade sulfide mineralization was related to the processes of late magmatic redeposition of ore matter under conditions of extensional deformations generated at the boundaries between rocks of contrasting compositions. It was shown that the formation of sulfides in amygdaloidal segregations could be related to the postmagmatic interaction of inclusion material with the host mineral.

M3 - Article

SP - 265

EP - 281

JO - Petrology

JF - Petrology

SN - 0869-5911

IS - 3

ER -

ID: 5054015