显微温度测试必须以油气包裹体鉴定为基础，单纯应用均一温度划分油气运移期次是不合适的。
It is not appropriate to classify the stages of petroleum migration only by applying homogenization temperatures of various inclusions.
利用显微红外光谱定性研究流体-熔融包裹体中的物相，其有机物不只是单一的甲烷相；
Micro-IR spectroscopy is used to analyze the components of the fluid-melt inclusion, in which organic matter is not unique methane phase.
用高倍荧光显微镜观察，在这些暗色泥岩的砂质碎屑矿物和自生矿物中，发现丰富的微石油包裹体群。
With high magnification of microscopy, a lot of petroleum inclusions were found, which occur in the fissures of sand grains and authigenic minerals in the source rock.
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