Informace o publikaci

Emerald from the Anuri Prospect, Nunavut, Canada

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GROAT Lee A. BRAND Allison CEMPÍREK Jan GRICE Joel WIGHT Willow

Rok publikování 2019
Druh Článek v odborném periodiku
Časopis / Zdroj Journal of Gemmology
Fakulta / Pracoviště MU

Přírodovědecká fakulta

Citace
www https://search.proquest.com/docview/2299784605/28E05AA8BE8045A1PQ/17?accountid=16531
Doi http://dx.doi.org/10.15506/JoG.2019.36.7.584
Klíčová slova Emerald; gemstone; gemology; Canada
Popis Ten polished thin sections of the seven intervals were studied with a petrographic microscope, scanning electron microscope and electron microprobe. The results show that the beryl occurs within a texturally and mineralogically variable matrix of phlogopite, muscovite, actinolite, plagioclase and pyrite, with occasional quartz, calcite and accessory minerals such as fluorapatite, titanite, rutile, chalcopyrite, molybdenite and rare tellurides. The beryl can occur as large, slightly altered grains in coarse-textured, hydrothermally altered, silicified zones, as well as at altered protolith contacts, as inclusions in other minerals (such as amphibole), and as a fine-grained, pervasive overprint that may represent a sodic alteration event.

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