热液生长绿柱石中一种新的流体包裹体类型

Rainer Thomas
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引用次数: 2

摘要

在绿柱石中发现了一种新的流体包裹体类型。包裹体主要由富水辉石组成,通过超临界流体或熔体从下地幔输送到上地壳结晶层。在此条件下,由于绿柱石的高溶解度,原生均一包裹体由于密度变化剧烈而分裂成两部分
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A New Fluid Inclusion Type in Hydrothermal-Grown Beryl
The formation of a new fluid inclusion type in beryl is shown. Primarily the inclusion was composed of water-rich stishovite, which was transported from the lower mantle into the upper crust crystallization level via a supercritical fluid or melt. After trapping and phase change, the primary homogeneous inclusion split due to drastic density changes into two parts by the high beryl solubility under such conditions
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