Fractionation in Li-tourmaline from the Lhenice lepidolite
pegmatite -

k 2017

Fractionation in Li-tourmaline from the Lhenice lepidolite pegmatite - "darrellhenryite loop" in F-saturation

SKŘÁPKOVÁ, Lenka; Jan CEMPÍREK a Michaela VAŠINOVÁ GALIOVÁ

Základní údaje

Originální název

Fractionation in Li-tourmaline from the Lhenice lepidolite pegmatite - "darrellhenryite loop" in F-saturation

Autoři

SKŘÁPKOVÁ, Lenka ; Jan CEMPÍREK a Michaela VAŠINOVÁ GALIOVÁ

Vydání

Tourmaline 2017, 2017

Další údaje

Jazyk

angličtina

Typ výsledku

Prezentace na konferencích

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Česká republika

Utajení

není předmětem státního či obchodního tajemství

Označené pro přenos do RIV

Ano

Kód RIV

RIV/00216224:14310/17:00097271

Organizační jednotka

Přírodovědecká fakulta

Klíčová slova anglicky

pegmatite; tourmaline; lepidolite; elbaite; darrellhenryite; fluorine

Příznaky

Mezinárodní význam

Změněno: 7. 3. 2018 09:38, doc. Mgr. Jan Cempírek, Ph.D.

Anotace

V originále

The lepidolite-subtype pegmatite at Lhenice, South Bohemia, Czech Republic, is a moderate-sized, highly fractionated pegmatite with abundant lepidolite, elbaite, amblygonite, and cassiterite. As the first mineralogical study at the locality, we acquired EMPA and LA-ICP-MS data of pink and colorless tourmaline from the most fractionated pegmatite units. When looking in detail at the tourmaline assemblages, we can conclude that the primary tourmaline (Tur 1) crystallized from Na-rich melt that produced abundant albite. The tourmaline crystallization overlaps with emergence of the first mica n the albite zone; we suggest that the sudden drop in the tourmaline F content was caused by start of mica crystallization. The F-depleted tourmaline (darrellhenryite) in the lepidolite core is also either coeval or slightly older than the associated lepidolite. The evolution path of the early tourmaline therefore follows a “loop” of Na,F decrease and increase, turning at darrellhenryite composition. Late development of the primary tourmaline is characterized by an increase in Na, OH, F and Fe contents. The new tourmaline generation (Tur 2) is associated by late K-feldspar and muscovite, suggesting hydrothermal crystallization. Textures of latest Fe-enriched (but not Mg- or Ca-bearing) fluor-elbaite (Tur 3) indicate hydrothermal origin; we suggest that its high Fe content might reflect composition of primary hydrothermal fluid in a closed system.

Návaznosti

MUNI/A/1653/2016, interní kód MU

Název: Geologické, geodynamické a environmentální procesy při východním okraji Českého masívu (Akronym: Geodyn)

Investor: Masarykova univerzita, Geologické, geodynamické a environmentální procesy při východním okraji Českého masívu, DO R. 2020_Kategorie A - Specifický výzkum - Studentské výzkumné projekty

Citovat

SKŘÁPKOVÁ, Lenka; Jan CEMPÍREK a Michaela VAŠINOVÁ GALIOVÁ. Fractionation in Li-tourmaline from the Lhenice lepidolite pegmatite - "darrellhenryite loop" in F-saturation. In Tourmaline 2017. 2017.

@proceedings{1386503,
   author = {Skřápková, Lenka and Cempírek, Jan and Vašinová Galiová, Michaela},
   booktitle = {Tourmaline 2017},
   keywords = {pegmatite; tourmaline; lepidolite; elbaite; darrellhenryite; fluorine},
   language = {eng},
   title = {Fractionation in Li-tourmaline from the Lhenice lepidolite pegmatite - "darrellhenryite loop" in F-saturation},
   year = {2017}
}

TY  - CONF
ID  - 1386503
AU  - Skřápková, Lenka - Cempírek, Jan - Vašinová Galiová, Michaela
PY  - 2017
TI  - Fractionation in Li-tourmaline from the Lhenice lepidolite pegmatite - "darrellhenryite loop" in F-saturation
KW  - pegmatite
KW  - tourmaline
KW  - lepidolite
KW  - elbaite
KW  - darrellhenryite
KW  - fluorine
N2  - The lepidolite-subtype pegmatite at Lhenice, South Bohemia, Czech Republic, is a moderate-sized, highly fractionated pegmatite with abundant lepidolite, elbaite, amblygonite, and cassiterite. As the first mineralogical study at the locality, we acquired EMPA and LA-ICP-MS data of pink and colorless tourmaline from the most fractionated pegmatite units. When looking in detail at the tourmaline assemblages, we can conclude that the primary tourmaline (Tur 1) crystallized from Na-rich melt that produced abundant albite. The tourmaline crystallization overlaps with emergence of the first mica n the albite zone; we suggest that the sudden drop in the tourmaline F content was caused by start of mica crystallization. The F-depleted tourmaline (darrellhenryite) in the lepidolite core is also either coeval or slightly older than the associated lepidolite. The evolution path of the early tourmaline therefore follows a “loop” of Na,F decrease and increase, turning at darrellhenryite composition. Late development of the primary tourmaline is characterized by an increase in Na, OH, F and Fe contents. The new tourmaline generation (Tur 2) is associated by late K-feldspar and muscovite, suggesting hydrothermal crystallization. Textures of latest Fe-enriched (but not Mg- or Ca-bearing) fluor-elbaite (Tur 3) indicate hydrothermal origin; we suggest that its high Fe content might reflect composition of primary hydrothermal fluid in a closed system.
ER  -

SKŘÁPKOVÁ, Lenka; Jan CEMPÍREK a Michaela VAŠINOVÁ GALIOVÁ. Fractionation in Li-tourmaline from the Lhenice lepidolite pegmatite - ''darrellhenryite loop'' in F-saturation. In \textit{Tourmaline 2017}. 2017.

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