A developmental model of olivine morphology as a function of the cooling rate and the degree of undercooling

被引:192
作者
Faure, F
Trolliard, G
Nicollet, C
Montel, JM
机构
[1] Univ Clermont Ferrand, Lab Magmas & Volcans, Observ Phys Globe Clermont Ferrand, UMR 6524,CNRS, F-63038 Clermont Ferrand, France
[2] CNRS, UMR 6638, F-87060 Limoges, France
[3] CNRS, Lab Mecanismes Transfert Geol Mineral, UMR 5563, CNRS, F-31000 Toulouse, France
关键词
D O I
10.1007/s00410-003-0449-y
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We performed dynamic crystallization experiments in the CMAS system at 1 atm to investigate the evolution of the morphology of forsterite crystals as a function of cooling rate and degree of undercooling. In sections parallel to the (010) plane, we observed the evolution of the forsterite morphology from tablets to hopper (skeletal) crystals, and then to swallowtail shapes (dendritic morphology) for increased degree of undercooling. The other shapes described in the literature can be interpreted as particular sections of those three shapes. The onset of dendritic growth is due to a competition between the growth of the faces of the initial hopper crystal and dendrite overgrowths. The forsterite dendrites are formed by a succession of units which look like hopper shapes. This result has been tested by an additional set of experiments.
引用
收藏
页码:251 / 263
页数:13
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