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 important prospecting criteria for K salt deposit are the fluid inclusion rich in K of mineral and rock, the hot spring rich in K and the saline lake rich in K.
矿物岩石流体包裹体的富钾成分、富钾热泉、富钾盐湖均是寻找钾盐矿床的重要指示。
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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