A new mineral facies has been found for the first time in mathiasite, resembling priderite in composition.
在辉石岩中首次发现了一种新的矿物相，其成分类似于柱红石。
The change of mineral facies is considered as one effect which affected on temperature to determine fluid inclusion by decrepitate.
矿物相的变化被认为是影响温度的一种影响，以决定岩屑是否包含流体。
The change of mineral facies is considered as one effect which affected on temperature determine of fluid inclusion by decrepitate.
矿物的相转变曾被认为是矿物包裹体爆裂法测温的影响因素之一。
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