Peridot from the Kugda Massif, Taymyr Region, Siberia.

  • Published In: Journal of Gemmology, 2024, v. 39, n. 1. P. 18 1 of 3

  • Database: Academic Search Ultimate 2 of 3

  • Authored By: Hanus, Radek 3 of 3

Abstract

The article discusses the discovery of peridot in the Kugda Massif in Siberia. The peridot veins are associated with desilicated pegmatites and zones of recrystallization. Gem-quality peridot is hosted by large clusters of clinohumite, phlogopite, and vermiculite, among other minerals. The peridot from the Kugda locality has not been previously characterized gemmologically and exhibits a yellowish-green color due to the presence of Fe2+. The quality and color of the peridot from this locality are comparable to peridot from other deposits, but the remoteness of the deposit and lack of infrastructure pose challenges for commercial viability. [Extracted from the article]

Additional Information

  • Source:Journal of Gemmology. 2024/01, Vol. 39, Issue 1, p18
  • Document Type:Article
  • Subject Area:Social Sciences and Humanities
  • Publication Date:2024
  • ISSN:1355-4565
  • DOI:10.15506/jog.2024.39.1.18
  • Accession Number:176621978
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