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光性礦物學.
光性礦物學(英語:optical mineralogy)
是通過測量礦物和岩石的光學特性來研究它們的一種技術。 最常見的是用偏光(polarized light)顯微鏡觀察岩石和礦物薄片。 光性礦物學用於鑒定礦物晶體和礦物組成,瞭解礦物和岩石的起源和演化。[1]
使用的一些屬性和技術包括[2]:
折射率、雙折射、Michel-Lévy干涉彩色图表、多色性、消光、錐光干涉圖、貝克線測試、光學浮凸、伸長的標誌(長度快與長度慢)[3]、波片。
- ^ Nesse, W.D. (1991). Introduction to Optical Mineralogy (2nd ed.). New York: Oxford University Press. p. 335. ISBN 0-19-506024-5.
- ^ Hartshorne, N. H.; Stuart, A. (1964). Practical Optical Crystallography. London: Edward Arnold. pp. 210–211.
- ^ Nelson, Stephen A. "Interference Phenomena, Compensation, and Optic Sign". EENS 2110: Mineralogy. Tulane University. Retrieved 24 March 2017
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