GENERATION AND RECRYSTALLIZATION OF DIAMONDS IN THE UPPER MANTLE

dc.contributor.author	Simakov S.K.
dc.date.accessioned	2020-04-13T10:51:03Z
dc.date.available	2020-04-13T10:51:03Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=30968735
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 301, 4, 157-160
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16692
dc.description.abstract	According to the meteoritic model of earth differentiation, liquid iron with carbon was generated in the initial period of differentiation. Thus, this event was close in time to the absolute age of the captive minerals of diamond and to the establishment of the ancient stable cratons and the beginning of outgassing of the mantle. The primary diamond nuclei were formed from melt containing liquid iron together with carbon in the early stages of planetary differentiation; subsequently, the diamonds probably experienced both solution and further growth from a fluid phase, with the extent of these processes depending on the concentration of nitrogen in the primary fluid.
dc.title	GENERATION AND RECRYSTALLIZATION OF DIAMONDS IN THE UPPER MANTLE
dc.type	Статья

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