Synthesis of pyrope-grossular garnets: an experimental study at P=2.5 GPa

被引:1
|
作者
Orlando, A
Borrini, D
机构
[1] CNR, Ist Geosci & Georisorse, Sezione Firenze, I-50121 Florence, Italy
[2] Univ Florence, Dipartimento Sci Terra, I-50121 Florence, Italy
关键词
D O I
10.1007/s00710-002-0223-2
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
In order to evaluate the stability of Mg-Ca garnets at P = 2.5 GPa/T = 800-1500degreesC, some experiments were performed using both natural and synthetic starting materials. Particular attention was paid to the investigation of the Ca rich side of the pyrope-grossular join and the maximum pyrope content in grossular was found to be about 10 mol. %. The addition of Cr to the system only slightly increases the observed pyrope solubility in grossular whereas Na stabilises melilite and merwinite. Clinopyroxene with a composition lying on the diopside-Ca Tschermak join appears to be the only stable crystalline phase in the middle part of the pyrope-grossular join.
引用
收藏
页码:37 / 51
页数:15
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