Four Treasures Reference Database
Record No. 5405
Different origins of Thai area sapphire and ruby, derived from mineral inclusions and co-existing minerals
Journal Article
Saminpanya, S. and Sutherland, F.L. (2011) Different origins of Thai area sapphire and ruby, derived from mineral inclusions and co-existing minerals. European Journal of Mineralogy, Vol. 23, No. 4, Aug.–Sept.,, 1-Aug-11 pp. 683–694.
DOI: https://dx.doi.org/10.1127/0935-1221/2011/0023-2123 | RWHL*
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corundum, inclusions.5, Thailand.12, Laos.12, gems
Mineral inclusions and coexisting minerals of gem corundum from the Thailand area analysed by SEM-EDS in this study can be divided into sapphire and ruby suites. The sapphire suite includes alkali feldspar (sanidine), nepheline, zircon, hercynite-spinel series and magnetite-hercynite series. The ruby suite includes garnet (pyrope), high-Al diopside ( fassaite') and sapphirine. The mineral chemistry and other data suggest that Thai rubies could have crystallized in high-pressure metamorphic rock of ultramafic/mafic composition. In contrast, Thai area sapphires could have crystallized in high-grade metamorphic (gneissic) rock or from magmas of highly alkaline composition, located at shallower levels in the lithosphere than those hosting the Thai rubies.
