根据显微镜下、红外光谱和X射线衍射的研究,表明块状水钙铝榴石玉的主要矿物成分是水钙铝榴石,并有含量不等的透辉石和方解石等。
The study on massive hydrogrossular by means of polar microscope, infrared spectra and Xray shows that it consists mainly of hydrogrossular, with a little amount of diopside and calcite.
本文主要论述块状矿石显微镜下矿物含量点测法的估计定律,以及此定律的简要证明、测量统计中最低限度样本容量的确定及误差范围。
In this paper, estimating law for mineral content, simple proof of the law and determining lowest sample size and error range in measure and statistics are discussed.
矿石中铁、锰矿物主要以粉末状和致密块状两种状态存在。
Iron and manganese in minerals mainly are existed in states of compact and lumpy powder.
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