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1·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。

2·Combined with the study of fluid inclusion, the stages of diagenesis are divided.

结合流体包裹体研究，进行了成岩作用阶段的划分。

3·This article cites Dongying Sag to analyze its paleopressure by using fluid inclusion.

文章以东营凹陷为例利用流体包裹体分析了其古压力。

4·Fluid inclusion contains pore fluid property and information on its geological history.

流体包裹体蕴含着孑乙隙流体性质及其在地质史中演变的信息。

5·Various gaseous composition of fluid inclusion represents different mineralization stages.

代表不同成矿阶段的包裹体气相组成有明显差异。

6·The researched fluid inclusion is in a CH4-H2O system identified by Raman spectroscopy at room temperature.

并由常温拉曼光谱分析表明，研究流体包裹体的流体组成为CH4-H2O体系。

7·The bubble of fluid inclusion is much bigger and the gas content is much higher at premetallogenetic period.

相山铀矿田成矿期前的流体包裹体中气泡较大，气体含量较高，表明包裹体捕获时压力较大；

8·The important prospecting criteria for K salt deposit are the fluid inclusion rich in K of mineral and rock, the hot spring ric…

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。

9·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。

10·This paper introduces an improvement on the preparatory technique for measurement of hydrogen isotope extracted from fluid inclusion.

本文介绍了改进测定流体包裹体氢同位素样品制样技术的一种方法。