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The Shape of Ekanite

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NASDALA Lutz SAMEERA K. A. Geeth FERNANDO G. W. A. Rohan WILDNER Manfred CHANMUANG Chutimun N. HABLER Gerlinde ERLACHER Annalena ŠKODA Radek

Rok publikování 2022
Druh Článek v odborném periodiku
Časopis / Zdroj Gems & Gemology
Fakulta / Pracoviště MU

Přírodovědecká fakulta

Citace
www http://dx.doi.org/10.5741/GEMS.58.2.156
Doi http://dx.doi.org/10.5741/GEMS.58.2.156
Klíčová slova ekanite; zircon; Sri Lankan; gem; shapes
Popis Despite its high thorium content, and consequent radioactivity, ekanite is still commonly traded in the Sri Lankan gem market. Gem-quality ekanite is derived from several gravel deposits in the country. However, rough specimens do not show rounded shapes that would be expected for stones transported by water; rather, they have remarkably uneven surfaces with multitudes of hollows, bumps, and cavities. Only after the recent discovery of ekanite in its host calc-silicate rock near Ampegama, Southern Province, can the striking shapes be understood. Fluid-driven alteration of ekanite, still inside the host rock, results in the formation of banded nodules with heterogeneous disintegration rims of an earthy consistency. These rims are readily removed by weathering, whereas the interior remnant consisting of chemically and physically resistant, unaltered ekanite persists.

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