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

dc.contributor.author	Semenov V.S.
dc.contributor.author	Semenov S.V.
dc.contributor.author	Zil'bershteǐn A.Kh.
dc.contributor.author	Korneev S.I.
dc.contributor.author	Kol'tsov A.B.
dc.contributor.author	Yakovleva O.A.
dc.contributor.author	Grinevich N.G.
dc.date.accessioned	2022-11-05T05:56:19Z
dc.date.available	2022-11-05T05:56:19Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13471325
dc.identifier.citation	Petrology, 2004, 12, 3, 265-281
dc.identifier.issn	0869-5911
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/39500
dc.description.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.
dc.title	DISTRIBUTION OF FE-NI-CU SULFIDE MINERALIZATION IN THE ROCKS OF THE BURAKOVSKO-AGANOZERSKIǐ LAYERED INTRUSION
dc.type	Статья

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