TEXTURAL EVOLUTION OF POLYHEDRAL OLIVINE EXPERIENCING RAPID COOLING RATES

dc.contributor.authorFaure F.
dc.contributor.authorSchiano P.
dc.contributor.authorNicollet C.
dc.contributor.authorTrolliard G.
dc.contributor.authorSoulestin B.
dc.date.accessioned2026-02-21T09:20:47Z
dc.date.issued2007
dc.description.abstractDynamic crystallization experiments in the CaO-MgO-Al2 O3-SiO2 (CMAS) system have been used to investigate the change in crystal shape when pre-existing polyhedral olivine crystals are cooled rapidly (1,639-2,182°C/h). Polyhedral olivines are crystallized initially in a first step using a slow cooling rate (2°C/h), then skeletal and dendritic overgrowths develop on the polyhedral crystals during a subsequent fast cooling event. During this second episode small dendritic olivines also nucleate within the liquid phase. Observation of the experimental sample by optical microscopy shows that the polyhedral olivine shape progressively changes to a skeletal and then to a dendritic morphology in the following sequence: polyhedral ⇒ hopper polyhedral ⇒ dendritic polyhedral. This evolutional sequence is discussed in terms of changes in the crystal growth conditions during cooling and a general relation between these olivine dynamic crystallization experiments and the integrated model of crystal growth by Sunagawa (Bull Minér 104:81-87, 1981 Morphology of crystals, Terra Scientific Publishing Company, 1987) is proposed. © Springer-Verlag 2006.
dc.identifierhttps://elibrary.ru/item.asp?id=31352258
dc.identifier.citationContributions to Mineralogy and Petrology, 2007, 153, 4, 405-416
dc.identifier.doi10.1007/s00410-006-0154-8
dc.identifier.issn0010-7999
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/51201
dc.subjectolivine
dc.titleTEXTURAL EVOLUTION OF POLYHEDRAL OLIVINE EXPERIENCING RAPID COOLING RATES
dc.typeСтатья

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