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直辉橄辉岩:高低温倒置。

Clinoenstatite: High-Low Inversion.

出版信息

Science. 1965 May 21;148(3673):1090-1. doi: 10.1126/science.148.3673.1090.

Abstract

Clinoenstatite undergoes a metastable displacive inversion at 995 degrees C. The new phase can be indexed (from x-ray powder pattern) on a triclinic cell with dimensions a = 10.00 A; b = 8.934 A; c = 5.170 A; alpha = 88.27 degrees ; beta = 70.03 degrees ; gamma = 91.09 degrees . The new phase persists from 995 degrees to 1010 degrees C at the composition MgSiO(3). For a solid solution (15 percent by weight) of diopside in clinoenstatite, the new phase persists from 995 degrees to at least 1400 degrees C and does not invert in periods of several hours to protoenstatite, the phase previously thought to be the stable form in this region.

摘要

斜顽辉石在 995°C 经历亚稳位移型反转。新相可以用一个三方晶胞的指标(来自 X 射线粉末图),晶胞参数为 a = 10.00 A;b = 8.934 A;c = 5.170 A;α = 88.27°;β = 70.03°;γ = 91.09°。新相在 MgSiO(3) 的组成下从 995°C 持续到 1010°C。对于斜顽辉石中透辉石的固溶体(重量 15%),新相从 995°C 持续到至少 1400°C,并且在数小时内不会反转成斜方顽辉石,之前认为斜方顽辉石是该区域的稳定相。

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