MATERIAL TRANSPORT IN LASER-HEATED DIAMOND ANVIL CELL MELTING EXPERIMENTS

被引:9
作者
CAMPBELL, AJ
HEINZ, DL
DAVIS, AM
机构
[1] UNIV CHICAGO,ENRICO FERMI INST,CHICAGO,IL 60637
[2] UNIV CHICAGO,JAMES FRANCK INST,CHICAGO,IL 60637
关键词
D O I
10.1029/92GL00972
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Olivine from San Carlos, Arizona, Fa0.093 was compressed in a diamond anvil cell and melted under the action of a Nd:YAG laser. Stripes of melted material wert formed by scanning the sample under the laser. Scanning electron microscopy and x-ray microanalysis of the recovered samples reveal large-scale (approximately 100-mu-m) transport of material through the sample, caused by the laser-induced melting. Early-crystallizing phases form at the beginning of the laser-melted stripe; incompatible elements and late-crystallizing phases am concentrated at the end of the stripe. This behavior is exploited to determine melting behavior of high-pressure silicate assemblages of olivine composition. At pressures where beta-spinel is the phase melted, relative strengths of partitioning can be estimated for the incompatible elements studied. Iron was found to partition into the melt from beta-spinel less strongly than calcium, and slightly more strongly than manganese. At higher pressures, where a silicate perovskite/magnesiowustite assemblage is melted, it is determined that silicate perovskite is the liquidus phase, with iron-rich magnesiowustite accumulating at the end of the laser-melted stripe.
引用
收藏
页码:1061 / 1064
页数:4
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