Fractionation of tourmaline in the Lhenice lepidolite pegmatite

Warning

This publication doesn't include Faculty of Sports Studies. It includes Faculty of Science. Official publication website can be found on muni.cz.

Authors	SKŘÁPKOVÁ Lenka CEMPÍREK Jan
Year of publication	2018
Type	Conference abstract
MU Faculty or unit	Faculty of Science
Citation
Description	The lepidolite-subtype pegmatite at Lhenice is a member of the South-Bohemian pegmatite field (Novák & 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.
Related projects:	Turmalín - indikátor geologických procesů Geologické, geodynamické a environmentální procesy východního okraje Českého masívu a jejich vývoj.