铍的地球化学:硬币的另一面

Rainer Thomas
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引用次数: 0

摘要

由于富水熔融包裹体在微观加热阶段由于包裹体内部压力的增大,在加热过程中表现出泄漏或衰减的趋势。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
To the Geochemistry of Beryllium: The Other Side of the Coin
technique because water-rich melt inclusions show the tendency to leak or decrepitate during heating on the microscopic heating stage due to the growing pressure inside the inclusions.
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