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矿物的标型性的现代概念是费尔斯曼引进到矿物学中来的。他在“伟晶岩”(1931)一书中划分出大约70种标型矿物,这些矿物反映伟晶作用的不同阶段。他还在1940年的著作中强调指出,应该把标型矿物和矿物的标型特征区别开来。标型矿物决定地球化学作用(地质相)发育的条件和时间,而矿物的标型特征或标型性质反映着矿物形成作用的某些特点。费尔斯曼认为,矿物的标型特征包括:化学成分、类质同象混入物的含量、颜色、晶体形态等的变化。
The modern concept of the typology of minerals comes from the introduction of Felsman into mineralogy. In his book, Pegmatite (1931), he drew out about 70 types of minerals that reflect the different phases of pegmatism. He also emphasized in his 1940 writings that the distinctive characteristics of the mark minerals and minerals should be distinguished. Geotectonic minerals determine the conditions and time for the development of geochemical processes (geologic facies), while the mineralization features or typologies reflect certain characteristics of mineral formation. According to Felsman, the mineralogical characteristics include the chemical composition, the content, the color, the change of the crystal morphology and the like of the isomorphous mixture.