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Fractionation of tourmaline in the Lhenice lepidolite pegmatite

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F18%3A00101089" target="_blank" >RIV/00216224:14310/18:00101089 - isvavai.cz</a>

  • Result on the web

  • DOI - Digital Object Identifier

Alternative languages

  • Result language

    angličtina

  • Original language name

    Fractionation of tourmaline in the Lhenice lepidolite pegmatite

  • Original language description

    The lepidolite-subtype pegmatite at Lhenice is a member of the South-Bohemian pegmatite field (Novák &amp; Cempírek, 2010); the nearest rare-element pegmatites include Lhenice II, Nová Ves and Chvalovice I and II. All pegmatites are characterized by high Li and P contents and similar mineral composition (elbaite, schorl, biotite, K-feldspar, lepidolite). The Lhenice pegmatite is moderate-sized and highly fractionated, with abundant lepidolite, elbaite, amblygonite and cassiterite. Tourmaline samples were analysed using EMPA and LA-ICP-MS. Primary, metasomatic and recrystallized tourmaline generations were characterized.

  • Czech name

  • Czech description

Classification

  • Type

    O - Miscellaneous

  • CEP classification

  • OECD FORD branch

    10504 - Mineralogy

Result continuities

  • Project

    <a href="/en/project/GA17-17276S" target="_blank" >GA17-17276S: Tourmaline – an indicator of geological processes</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2018

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů