Chhong-ge̍k
Chhong-ge̍k[1] (蒼玉; Eng-gí: chalcedony) mā thang kóng sī gio̍k-chhé (玉髓, chham-khó Hôa-gí 玉髓, Ji̍t-gí 玉髄), sī ê ún-cheng-chit, sī sè-sè-lia̍p chio̍h-eng kah moganite ê liân-cheng (連晶; intergrowth).[2]
Chham-khó chu-liāu
[siu-kái | kái goân-sí-bé]- ↑ Embree, Bernard L.M. "chhong-ge̍k". A Dictionary of Southern Min [Embree Tâi Eng Sû-tián]. Hiong-káng: Hiong-káng Gí-giân Ha̍k-īⁿ. p. 61.
- ↑ Heaney, Peter J. (1994). "Structure and Chemistry of the low-pressure silica polymorphs". Chū Heaney, P. J.; Prewitt, C. T.; Gibbs, G. V. Silica: Physical Behavior, geochemistry and materials applications. Reviews in Mineralogy. 29. pp. 1–40.
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