释义 |
adulariaenUK
ad·u·lar·i·a A0100300 (ăj′ə-lâr′ē-ə, -lăr′-)n. A colorless to milky white mineral of the potassium feldspar group that forms from relatively low-temperature magmas and lacks structural homogeneity. [Italian, from French adulaire, after Adula, a mountain group of southeast Switzerland.]adularia (ˌædjʊˈlɛərɪə) n (Minerals) a white or colourless glassy variety of orthoclase in the form of prismatic crystals. It occurs in metamorphic rocks and is a minor gemstone. Formula: KAlSi3O8[C18: via Italian from French adulaire, after Adula, a group of mountains in Switzerland]ad•u•lar•i•a (ˌædʒ əˈlɛər i ə) n., pl. -lar•i•as. a sometimes opalescent variety of orthoclase formed at a low temperature. [1790–1800; < Italian < French adulaire, after Adula a mountain group in Switzerland; see -ary] adulariaenUK
adularia[‚aj·ə′la·rē·ə] (mineralogy) A weakly triclinic form of the mineral orthoclase occurring in transparent, colorless to milky-white pseudo-orthorhombic crystals. |