Alpine oxidation of lithium micas in Permian S-type granites
(Gemeric unit, Western Carpathians, Slovakia)

J 2014

Alpine oxidation of lithium micas in Permian S-type granites (Gemeric unit, Western Carpathians, Slovakia)

PETŘÍK, I., M. ČÍK, M. MIGLIERINI, Tomáš VACULOVIČ, I. DIANIŠKA et. al.

Základní údaje

Originální název

Alpine oxidation of lithium micas in Permian S-type granites (Gemeric unit, Western Carpathians, Slovakia)

Autoři

PETŘÍK, I. (703 Slovensko, garant), M. ČÍK (703 Slovensko), M. MIGLIERINI (703 Slovensko), Tomáš VACULOVIČ (703 Slovensko, domácí), I. DIANIŠKA (703 Slovensko) a D. OZDÍN (703 Slovensko)

Vydání

Mineralogical Magazine, Middlesex, Mineralogical Society, 2014, 0026-461X

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10406 Analytical chemistry

Stát vydavatele

Česká republika

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 2.026

Kód RIV

RIV/00216224:14740/14:00079354

Organizační jednotka

Středoevropský technologický institut

DOI

http://dx.doi.org/10.1180/minmag.2014.078.3.03

UT WoS

000344420400003

Klíčová slova anglicky

lithium micas; zinnwaldite; phengite; Permian granite; oxidation; Alpine metamorphism; Gemeric unit; Western Carpathians; Slovakia

Štítky

kontrola MP, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 18. 3. 2015 09:41, doc. Mgr. Tomáš Vaculovič, Ph.D.

Anotace

V originále

Lithium micas of the zinnwaldite and phengite-Li-phengite series occur as characteristic minerals in Permian Li-F-(P) granites of the western Gemeric unit (Western Carpathians) accompanied by topaz, tourmaline, Nb, Ta, Ti, Sn oxides and aluminophosphates. The calculated Li2O contents of all the mica analysed, together with Rb2O and Cs2O were confirmed by LA-ICP-MS analyses for all the identified micas. Samples from three localities were investigated: two surficial (Surovec, Vrchsul'ova); and one drill hole (Dlha dolina). Zinnwaldite (polylithionite) occurs in the upper level of the Dlha dolina granitic intrusion and in the nearby shallow satellite body of Surovec. The lower level porphyritic granites contain only siderophyllite. The Vrchsul'ova micas are closer in composition to Li-annite and siderophyllite. Dioctahedral micas are mostly phengites, although zinnwaldite-bearing granites are rich in late-crystallizing Li-phengite, which extensively replaces earlier zinnwaldite. The secondary Li-phengite and phengite are interpreted as products of Alpine metamorphism during Cretaceous burial and subsequent exhumation of the Gemeric unit. Reactions are suggested explaining the formation of Li-phengite by reaction of zinnwaldite with phengite or with muscovite. All mica types were investigated by Mossbauer spectroscopy, which showed high degrees of oxidation (25-50% Fe3+ of total Fe) with the exception of zinnwaldite from Vrchsul'ova, which may have preserved an original, reduced value of 10%. The metamorphic assemblage present permitted calculation of P-T-X conditions: T = 184 degrees C, P = 320 MPa, with oxidation of siderophyllite to phengite + goethite and f(O2) at Delta NN = 4.7, confirming the low-grade conditions of the Alpine metamorphism in agreement with previous estimates.

Citovat

PETŘÍK, I., M. ČÍK, M. MIGLIERINI, Tomáš VACULOVIČ, I. DIANIŠKA a D. OZDÍN. Alpine oxidation of lithium micas in Permian S-type granites (Gemeric unit, Western Carpathians, Slovakia). Mineralogical Magazine. Middlesex: Mineralogical Society, 2014, roč. 78, č. 3, s. 507-533. ISSN 0026-461X. Dostupné z: https://dx.doi.org/10.1180/minmag.2014.078.3.03.

@article{1228990,
   author = {Petřík, I. and Čík, M. and Miglierini, M. and Vaculovič, Tomáš and Dianiška, I. and Ozdín, D.},
   article_location = {Middlesex},
   article_number = {3},
   doi = {http://dx.doi.org/10.1180/minmag.2014.078.3.03},
   keywords = {lithium micas; zinnwaldite; phengite; Permian granite; oxidation; Alpine metamorphism; Gemeric unit; Western Carpathians; Slovakia},
   language = {eng},
   issn = {0026-461X},
   journal = {Mineralogical Magazine},
   title = {Alpine oxidation of lithium micas in Permian S-type granites (Gemeric unit, Western Carpathians, Slovakia)},
   url = {http://minmag.geoscienceworld.org/content/78/3/507.abstract},
   volume = {78},
   year = {2014}
}

TY  - JOUR
ID  - 1228990
AU  - Petřík, I. - Čík, M. - Miglierini, M. - Vaculovič, Tomáš - Dianiška, I. - Ozdín, D.
PY  - 2014
TI  - Alpine oxidation of lithium micas in Permian S-type granites (Gemeric unit, Western Carpathians, Slovakia)
JF  - Mineralogical Magazine
VL  - 78
IS  - 3
SP  - 507-533
EP  - 507-533
PB  - Mineralogical Society
SN  - 0026461X
KW  - lithium micas
KW  - zinnwaldite
KW  - phengite
KW  - Permian granite
KW  - oxidation
KW  - Alpine metamorphism
KW  - Gemeric unit
KW  - Western Carpathians
KW  - Slovakia
UR  - http://minmag.geoscienceworld.org/content/78/3/507.abstract
L2  - http://minmag.geoscienceworld.org/content/78/3/507.abstract
N2  - Lithium micas of the zinnwaldite and phengite-Li-phengite series occur as characteristic minerals in Permian Li-F-(P) granites of the western Gemeric unit (Western Carpathians) accompanied by topaz, tourmaline, Nb, Ta, Ti, Sn oxides and aluminophosphates. The calculated Li2O contents of all the mica analysed, together with Rb2O and Cs2O were confirmed by LA-ICP-MS analyses for all the identified micas. Samples from three localities were investigated: two surficial (Surovec, Vrchsul'ova); and one drill hole (Dlha dolina). Zinnwaldite (polylithionite) occurs in the upper level of the Dlha dolina granitic intrusion and in the nearby shallow satellite body of Surovec. The lower level porphyritic granites contain only siderophyllite. The Vrchsul'ova micas are closer in composition to Li-annite and siderophyllite. Dioctahedral micas are mostly phengites, although zinnwaldite-bearing granites are rich in late-crystallizing Li-phengite, which extensively replaces earlier zinnwaldite. The secondary Li-phengite and phengite are interpreted as products of Alpine metamorphism during Cretaceous burial and subsequent exhumation of the Gemeric unit. Reactions are suggested explaining the formation of Li-phengite by reaction of zinnwaldite with phengite or with muscovite. All mica types were investigated by Mossbauer spectroscopy, which showed high degrees of oxidation (25-50% Fe3+ of total Fe) with the exception of zinnwaldite from Vrchsul'ova, which may have preserved an original, reduced value of 10%. The metamorphic assemblage present permitted calculation of P-T-X conditions: T = 184 degrees C, P = 320 MPa, with oxidation of siderophyllite to phengite + goethite and f(O2) at Delta NN = 4.7, confirming the low-grade conditions of the Alpine metamorphism in agreement with previous estimates.
ER  -

PETŘÍK, I., M. ČÍK, M. MIGLIERINI, Tomáš VACULOVIČ, I. DIANIŠKA a D. OZDÍN. Alpine oxidation of lithium micas in Permian S-type granites (Gemeric unit, Western Carpathians, Slovakia). \textit{Mineralogical Magazine}. Middlesex: Mineralogical Society, 2014, roč.~78, č.~3, s.~507-533. ISSN~0026-461X. Dostupné z: https://dx.doi.org/10.1180/minmag.2014.078.3.03.

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