TEXTURAL EVOLUTION OF POLYHEDRAL OLIVINE EXPERIENCING RAPID COOLING RATES
| dc.contributor.author | Faure F. | |
| dc.contributor.author | Schiano P. | |
| dc.contributor.author | Nicollet C. | |
| dc.contributor.author | Trolliard G. | |
| dc.contributor.author | Soulestin B. | |
| dc.date.accessioned | 2026-02-21T09:20:47Z | |
| dc.date.issued | 2007 | |
| dc.description.abstract | Dynamic 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.identifier | https://elibrary.ru/item.asp?id=31352258 | |
| dc.identifier.citation | Contributions to Mineralogy and Petrology, 2007, 153, 4, 405-416 | |
| dc.identifier.doi | 10.1007/s00410-006-0154-8 | |
| dc.identifier.issn | 0010-7999 | |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/51201 | |
| dc.subject | olivine | |
| dc.title | TEXTURAL EVOLUTION OF POLYHEDRAL OLIVINE EXPERIENCING RAPID COOLING RATES | |
| dc.type | Статья |
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