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以显微照片方式报道了对大冶铁矿床夕卡岩矿物中熔融包裹体、熔-流包裹体和流体包裹体的观察结果和对包裹体相态特征的研究结果。结果表明，在所研究的包裹体中，矿物熔融包裹体最为常见，偶见熔-流包裹体和流体包裹体。熔融包裹体在大冶铁矿床夕卡岩矿物中不仅存在而且广泛分布，在偏光显微镜下很容易找到。熔融包裹体的存在对夕卡岩传统的接触交代成因观点具有挑战性，有助于夕卡岩和夕卡岩矿床成因理论研究水平的提高。
The results of observations on melt inclusions, melt-flow inclusions and fluid inclusions in the skarn minerals from the Daye iron deposit and the phase characterization of the inclusions are reported by photomicrographs. The results show that, in the study of inclusions, mineral melt inclusions are the most common, occasionally melt-flow inclusions and fluid inclusions. The melt inclusions are not only present but widely distributed in the skarn minerals of Daye iron deposit, which can be easily found under a polarizing microscope. The existence of melt inclusions is challenging for the traditional explanation of the origin of skarn, and contributes to the study of the genetic theory of skarn and skarn deposits.