SKŘÁPKOVÁ, Lenka and Jan CEMPÍREK. The role of oxy-tourmalines and metasomatic mixing in evolution of lepidolite-subtype pegmatites. In TUR2021 3rd International Conference on Tourmaline. 2021.
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Basic information
Original name The role of oxy-tourmalines and metasomatic mixing in evolution of lepidolite-subtype pegmatites
Authors SKŘÁPKOVÁ, Lenka and Jan CEMPÍREK.
Edition TUR2021 3rd International Conference on Tourmaline, 2021.
Other information
Original language English
Type of outcome Presentations at conferences
Field of Study 10504 Mineralogy
Country of publisher Italy
Confidentiality degree is not subject to a state or trade secret
Organization unit Faculty of Science
Tags International impact, Reviewed
Changed by Changed by: Mgr. Lenka Skřápková, učo 434347. Changed: 8/11/2021 13:29.
Abstract
The lepidolite-subtype Lhenice pegmatite is a member of the South Bohemian pegmatite field in the is located in the southern part of the Moldanubian Zone of the Bohemian Massif, Czech Republic. We present results of textural and mineralogical analysis combined with data acquired using electron microprobe and LA-ICP-MS. The tourmaline in the Lhenice pegmatite shows apparently gradual evolution from the pegmatite border to its core from the most primitive to the most fractionated, with significant presence of oxy-tourmaline in all pegmatite zones. Tourmaline evolution is characterized by the crystallization of two primary tourmaline groups that, together with metasomatic generations, form the apparently continuous trend described by Selway et al. (1999). Study of the Lhenice pegmatite revealed complex evolution of tourmaline, mica and other accessory minerals that were very significantly affected by metasomatic and hydrothermal processes.
Links
GA19-05198S, research and development projectName: Greisenizace a albitizace - geologické procesy s potenciálem koncentrovat některé kritické suroviny pro moderní technologie (Acronym: GREISEN)
Investor: Czech Science Foundation
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