钙长石
透辉石
液相线
共晶体系
矿物学
热力学
地质学
相(物质)
猝灭(荧光)
三斜晶系
材料科学
化学
结晶学
冶金
晶体结构
物理
光学
微观结构
荧光
有机化学
作者
E. Christiaan de Wys,W. Foster
出处
期刊:Mineralogical magazine and journal of the Mineralogical Society
[The Mineralogical Society]
日期:1958-03-01
卷期号:31 (240): 736-743
被引量:13
标识
DOI:10.1180/minmag.1958.031.240.03
摘要
Summary The high-temperature phase equilibrium relationships in the system diopside-anorthite—åkermanite have been investigated by the quenching method. This system may be regarded as essentially a simple eutectic system. The eutectic is located at the composition 9 diopside:44 anorthite:47 åkermanite (by weight) and at a temperature of 1226° C. Åkermanite is a stable phase at least as low as this temperature. Triclinic anorthite is the only form of CaAl 2 Si 2 O 8 encountered in the liquidus range of temperatures.
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