Compositional and textural variations of columbite-group
minerals from beryl-columbite pegmatites in the Maršíkov
District, Bohemian Massif, Czech Republic: Magmatic versus
hydrothermal evolution

J 2020

Compositional and textural variations of columbite-group minerals from beryl-columbite pegmatites in the Maršíkov District, Bohemian Massif, Czech Republic: Magmatic versus hydrothermal evolution

CHLÁDEK, Štěpán; Pavel UHER a Milan NOVÁK

Základní údaje

Originální název

Compositional and textural variations of columbite-group minerals from beryl-columbite pegmatites in the Maršíkov District, Bohemian Massif, Czech Republic: Magmatic versus hydrothermal evolution

Autoři

CHLÁDEK, Štěpán (garant); Pavel UHER a Milan NOVÁK (203 Česká republika, domácí)

Vydání

Canadian Mineralogist, Mineralogical Association of Canada, 2020, 0008-4476

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10504 Mineralogy

Stát vydavatele

Kanada

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 1.165

Kód RIV

RIV/00216224:14310/20:00118967

Organizační jednotka

Přírodovědecká fakulta

DOI

https://doi.org/10.3749/canmin.1900093

UT WoS

000637945400007

EID Scopus

2-s2.0-85099051595

Klíčová slova anglicky

columbite-tantalite; compositional trends; granitic pegmatites

Štítky

rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 13. 5. 2021 18:51, Mgr. Marie Novosadová Šípková, DiS.

Anotace

V originále

We studied compositional variations in columbite group minerals (CGM) from several granitic pegmatites of the beryl-columbite subtype in the Maršíkov district, Silesian Domain of the Bohemian Massif, Czech Republic. The CGM are characterized by distinct zoned patterns in BSE images. Primary magmatic homogeneous to oscillatory zoning is preserved in corroded crystal cores, whereas the majority of the crystal volume is replaced by secondary complexly zoned domains formed via post-magmatic processes. The primary domains show relatively uniform evolutionary trends from core to rim, generally with steeply increasing Ta/(Ta + Nb) and negligible to slightly increasing Mn/(Mn + Fe). In contrast, the compositions of secondary CGM domains indicate a reversed evolution, with: (1) steeply decreasing Ta/(Ta + Nb) and relatively constant Mn/(Mn + Fe) characteristics for CGM in the Bienergraben and Scheibengraben pegmatites, and (2) insignificantly decreasing Ta/(Ta + Nb) and strongly decreasing Mn/(Mn + Fe) characteristics for CGM in the Schinderhübel I and Lysá Hora pegmatites. Patchy zoning and secondary evolution in CGM result from metasomatic replacement processes related to fluids. These fluids are probably late-magmatic and exsolved from the residual melt and in later stages locally mixed with external Mg-enriched fluids derived from the host rocks. The presence of volatiles (mainly H2O, F) facilitated high mobility of the elements and replacement of the early CGM. Textural characteristics and compositional variations in CGM show the complex evolution of the pegmatite system from the magmatic stage to subsolidus-hydrothermal conditions.

Návaznosti

GA19-05198S, projekt VaV

Název: Greisenizace a albitizace - geologické procesy s potenciálem koncentrovat některé kritické suroviny pro moderní technologie (Akronym: GREISEN)

Investor: Grantová agentura ČR, Greisenizace a albitizace - geologické procesy s potenciálem koncentrovat některé kritické suroviny pro moderní technologie

Citovat

CHLÁDEK, Štěpán; Pavel UHER a Milan NOVÁK. Compositional and textural variations of columbite-group minerals from beryl-columbite pegmatites in the Maršíkov District, Bohemian Massif, Czech Republic: Magmatic versus hydrothermal evolution. Canadian Mineralogist. Mineralogical Association of Canada, 2020, roč. 58, č. 6, s. 767-783. ISSN 0008-4476. Dostupné z: https://doi.org/10.3749/canmin.1900093.

@article{1768106,
   author = {Chládek, Štěpán and Uher, Pavel and Novák, Milan},
   article_number = {6},
   doi = {https://doi.org/10.3749/canmin.1900093},
   keywords = {columbite-tantalite; compositional trends; granitic pegmatites},
   language = {eng},
   issn = {0008-4476},
   journal = {Canadian Mineralogist},
   title = {Compositional and textural variations of columbite-group minerals from beryl-columbite pegmatites in the Maršíkov District, Bohemian Massif, Czech Republic: Magmatic versus hydrothermal evolution},
   url = {https://doi.org/10.3749/canmin.1900093},
   volume = {58},
   year = {2020}
}

TY  - JOUR
ID  - 1768106
AU  - Chládek, Štěpán - Uher, Pavel - Novák, Milan
PY  - 2020
TI  - Compositional and textural variations of columbite-group minerals from beryl-columbite pegmatites in the Maršíkov District, Bohemian Massif, Czech Republic: Magmatic versus hydrothermal evolution
JF  - Canadian Mineralogist
VL  - 58
IS  - 6
SP  - 767-783
EP  - 767-783
PB  - Mineralogical Association of Canada
SN  - 00084476
KW  - columbite-tantalite
KW  - compositional trends
KW  - granitic pegmatites
UR  - https://doi.org/10.3749/canmin.1900093
N2  - We studied compositional variations in columbite group minerals (CGM) from several granitic pegmatites of the beryl-columbite subtype in the Maršíkov district, Silesian Domain of the Bohemian Massif, Czech Republic. The CGM are characterized by distinct zoned patterns in BSE images. Primary magmatic homogeneous to oscillatory zoning is preserved in corroded crystal cores, whereas the majority of the crystal volume is replaced by secondary complexly zoned domains formed via post-magmatic processes. The primary domains show relatively uniform evolutionary trends from core to rim, generally with steeply increasing Ta/(Ta + Nb) and negligible to slightly increasing Mn/(Mn + Fe). In contrast, the compositions of secondary CGM domains indicate a reversed evolution, with: (1) steeply decreasing Ta/(Ta + Nb) and relatively constant Mn/(Mn + Fe) characteristics for CGM in the Bienergraben and Scheibengraben pegmatites, and (2) insignificantly decreasing Ta/(Ta + Nb) and strongly decreasing Mn/(Mn + Fe) characteristics for CGM in the Schinderhübel I and Lysá Hora pegmatites. Patchy zoning and secondary evolution in CGM result from metasomatic replacement processes related to fluids. These fluids are probably late-magmatic and exsolved from the residual melt and in later stages locally mixed with external Mg-enriched fluids derived from the host rocks. The presence of volatiles (mainly H2O, F) facilitated high mobility of the elements and replacement of the early CGM. Textural characteristics and compositional variations in CGM show the complex evolution of the pegmatite system from the magmatic stage to subsolidus-hydrothermal conditions.
ER  -

CHLÁDEK, Štěpán; Pavel UHER a Milan NOVÁK. Compositional and textural variations of columbite-group minerals from beryl-columbite pegmatites in the Maršíkov District, Bohemian Massif, Czech Republic: Magmatic versus hydrothermal evolution. \textit{Canadian Mineralogist}. Mineralogical Association of Canada, 2020, roč.~58, č.~6, s.~767-783. ISSN~0008-4476. Dostupné z: https://doi.org/10.3749/canmin.1900093.

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