Geochemistry of the ultramafites of the Guli platiniferous intrusion, Maymecha-Kotuy Province

V. G. Lazarenkov; K. N. Malich; G. G. Lopatin

Geochemistry of the ultramafites of the Guli platiniferous intrusion, Maymecha-Kotuy Province

V. G. Lazarenkov, K. N. Malich, G. G. Lopatin

ARC Centre of Excellence for Core to Crust Fluid Systems (incorporation ARC National Key Centre for Geochemical evolution and Metallogeny of Continents (GEMOC))

Research output: Contribution to journal › Article › peer-review

Abstract

The mean contents of the petrogenetic and trace elements, including the platinoids, in the main ultramafite varieties of the Guli intrusion are given. The slightly serpentinized dunites and chromitites are specialized in the refractory platinoids; the main platinoid in the clinopyroxenites and meymechites is palladium. The dunites include slightly serpentinized, serpentinized, and highly serpentinized varieties. It is concluded that during dunite serpentinization depletion in the refractory platinoids occurred, along with accumulation of palladium and the heavy lanthanoids.

Original language	English
Pages (from-to)	1-9
Number of pages	9
Journal	Geochemistry International
Volume	31
Issue number	6
Publication status	Published - 1994

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abstract = "The mean contents of the petrogenetic and trace elements, including the platinoids, in the main ultramafite varieties of the Guli intrusion are given. The slightly serpentinized dunites and chromitites are specialized in the refractory platinoids; the main platinoid in the clinopyroxenites and meymechites is palladium. The dunites include slightly serpentinized, serpentinized, and highly serpentinized varieties. It is concluded that during dunite serpentinization depletion in the refractory platinoids occurred, along with accumulation of palladium and the heavy lanthanoids.",

author = "Lazarenkov, {V. G.} and Malich, {K. N.} and Lopatin, {G. G.}",

year = "1994",

language = "English",

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journal = "Geochemistry International",

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AU - Malich, K. N.

AU - Lopatin, G. G.

PY - 1994

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N2 - The mean contents of the petrogenetic and trace elements, including the platinoids, in the main ultramafite varieties of the Guli intrusion are given. The slightly serpentinized dunites and chromitites are specialized in the refractory platinoids; the main platinoid in the clinopyroxenites and meymechites is palladium. The dunites include slightly serpentinized, serpentinized, and highly serpentinized varieties. It is concluded that during dunite serpentinization depletion in the refractory platinoids occurred, along with accumulation of palladium and the heavy lanthanoids.

AB - The mean contents of the petrogenetic and trace elements, including the platinoids, in the main ultramafite varieties of the Guli intrusion are given. The slightly serpentinized dunites and chromitites are specialized in the refractory platinoids; the main platinoid in the clinopyroxenites and meymechites is palladium. The dunites include slightly serpentinized, serpentinized, and highly serpentinized varieties. It is concluded that during dunite serpentinization depletion in the refractory platinoids occurred, along with accumulation of palladium and the heavy lanthanoids.

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M3 - Article

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JO - Geochemistry International

JF - Geochemistry International

IS - 6

ER -

Geochemistry of the ultramafites of the Guli platiniferous intrusion, Maymecha-Kotuy Province

Abstract

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