CHEMISTRY, SMALL-SCALE INHOMOGENEITY, AND FORMATION OF MOLDAVITES AS CONDENSATES FROM SANDS VAPORIZED BY THE RIES IMPACT

dc.contributor.author	von Engelhardt W.
dc.contributor.author	Berthold C.
dc.contributor.author	Wenzel T.
dc.contributor.author	Dehner T.
dc.date.accessioned	2023-11-12T04:40:04Z
dc.date.available	2023-11-12T04:40:04Z
dc.date.issued	2005
dc.identifier	https://www.elibrary.ru/item.asp?id=12092010
dc.identifier.citation	Geochimica et Cosmochimica Acta, 2005, 69, 23, 5611-5626
dc.identifier.issn	0016-7037
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/41672
dc.description.abstract	The formation of the Ries impact and the moldavites have identical radiogenic ages of 14.3 Ma. According to this conformity in age moldavites are generally regarded as products of the Ries impact. This paper, which is divided into two sections, deals with two aspects of the moldavite-forming process: the formation of moldavite bodies by accretion of small precursors, and the physical and chemical conditions under which these primary units originated from sands which covered the Ries impact site.
dc.title	CHEMISTRY, SMALL-SCALE INHOMOGENEITY, AND FORMATION OF MOLDAVITES AS CONDENSATES FROM SANDS VAPORIZED BY THE RIES IMPACT
dc.type	Статья
dc.identifier.doi	10.1016/j.gca.2005.07.004

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