Amphibole and pyroxene as indicators of alkaline conditions in
banded carbonatite-like marbles from Bližná, Český Krumlov
Unit, Moldanubian Zone

J 2021

Amphibole and pyroxene as indicators of alkaline conditions in banded carbonatite-like marbles from Bližná, Český Krumlov Unit, Moldanubian Zone

RADKOVÁ, Pavlína; Milan NOVÁK; Jan CEMPÍREK; Stanislav HOUZAR; Radek ŠKODA et. al.

Základní údaje

Originální název

Amphibole and pyroxene as indicators of alkaline conditions in banded carbonatite-like marbles from Bližná, Český Krumlov Unit, Moldanubian Zone

Autoři

RADKOVÁ, Pavlína (703 Slovensko, domácí); Milan NOVÁK (203 Česká republika, domácí); Jan CEMPÍREK (203 Česká republika, domácí); Stanislav HOUZAR a Radek ŠKODA (203 Česká republika, domácí)

Vydání

Journal of Geosciences, Czech Geological Society, 2021, 1802-6222

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10504 Mineralogy

Stát vydavatele

Česká republika

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 1.778

Kód RIV

RIV/00216224:14310/21:00119494

Organizační jednotka

Přírodovědecká fakulta

DOI

https://doi.org/10.3190/jgeosci.336

UT WoS

000738385300008

EID Scopus

2-s2.0-85122095441

Klíčová slova anglicky

Bohemian Massif; Moldanubian Zone; Český Krumlov Unit; pyroxene; alkali amphibole; carbonatite-like marble

Štítky

rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 31. 1. 2022 16:44, Mgr. Marie Novosadová Šípková, DiS.

Anotace

V originále

Amphiboles and diopside occur in several distinct mineral assemblages in banded carbonatite-like marbles from the Bližná graphite mine, Český Krumlov Unit, Moldanubian Zone. The carbonatite-like marble is interlayered with dominant ordinary metacarbonates as a single continuous stratabound layer, up to 3-4 m thick. It is enriched in elements typical for carbonatites (REE, Y, Th, Sr, Nb, Zr, and Mo) and contains accessory betafite-pyrochlore and uranothorite along with molybdenite, sulfides (e.g., pyrite, pyrrhotite) and oxides (e.g., magnetite, ilmenite). Detailed study of thin sections in optical microscope and BSE images as well as results of EMPA revealed three distinct mineral assemblages - richterite + forsterite (RF) assemblage (Rht + Fo + Cal ˃ Dol ˃ Phl + Di), Na rich actinolite + diopside (AD) assemblage (Di + Act + Rht + Cal ˃ Phl) and magnesio-hastingsite + diopside (HD) assemblage (Mhst + Di + Cal ˃ Ab + Phl). The distinct amphibole species found within the individual assemblages exhibit complex textural relations and crystallized in several prograde and retrograde stages. The following amphibole species were recognized in the individual assemblages: RF - (richterite > ferri-winchite > tremolite, edenite), AD - (actinolite > ferri-winchite; richterite > ferri-katophorite; magnesio-riebeckite), HD - (magnesio-hastingsite; ferri-winchite, actinolite). They differ especially in Mg/(Mg + Fetot) ratio and concentrations of F. Diopside contains up to 17 mol. % of the aegirine component and albite is Fe, Ba-enriched (≥ 0.69 wt. % BaO and ≥ 0.50 wt. % Fe2O3tot). The composition of amphiboles and pyroxenes indicates the alkaline environment of their formation; unusually high Fe2O3 contents in albite plagioclase have known counterparts in alkaline pegmatites and some carbonatite dykes. The following options of potential origin of the carbonatite-like marble from Bližná are discussed: (i) metacarbonates potentially with Na- and Na,Ca-carbonates and sulfate admixture; (ii) admixture of alkaline volcanodetritic component during carbonate sedimentation; (iii) metamorphosed carbonatites enclosed in ordinary sedimentary metacarbonate; (iv) Na-rich metasomatites characterized by mineral assemblages with Na,Fe,F-enriched amphiboles, diopside with high aegirine component and albite. With regard to the observed mineral assemblages, textures and composition of minerals, we can exclude (i) marine evaporates, whereas the other options (ii), (iii) and (iv) are, in general, possible. The amphiboles observed in the Bližná carbonatite-like marble are unique within the Bohemian Massif and distinctly different from amphiboles found in metacarbonates with evaporite component.

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

RADKOVÁ, Pavlína; Milan NOVÁK; Jan CEMPÍREK; Stanislav HOUZAR a Radek ŠKODA. Amphibole and pyroxene as indicators of alkaline conditions in banded carbonatite-like marbles from Bližná, Český Krumlov Unit, Moldanubian Zone. Journal of Geosciences. Czech Geological Society, 2021, roč. 66, č. 4, s. 243-262. ISSN 1802-6222. Dostupné z: https://doi.org/10.3190/jgeosci.336.

@article{1816399,
   author = {Radková, Pavlína and Novák, Milan and Cempírek, Jan and Houzar, Stanislav and Škoda, Radek},
   article_number = {4},
   doi = {https://doi.org/10.3190/jgeosci.336},
   keywords = {Bohemian Massif; Moldanubian Zone; Český Krumlov Unit; pyroxene; alkali amphibole; carbonatite-like marble},
   language = {eng},
   issn = {1802-6222},
   journal = {Journal of Geosciences},
   title = {Amphibole and pyroxene as indicators of alkaline conditions in banded carbonatite-like marbles from Bližná, Český Krumlov Unit, Moldanubian Zone},
   url = {http://www.jgeosci.org/detail/jgeosci.336/abstract/},
   volume = {66},
   year = {2021}
}

TY  - JOUR
ID  - 1816399
AU  - Radková, Pavlína - Novák, Milan - Cempírek, Jan - Houzar, Stanislav - Škoda, Radek
PY  - 2021
TI  - Amphibole and pyroxene as indicators of alkaline conditions in banded carbonatite-like marbles from Bližná, Český Krumlov Unit, Moldanubian Zone
JF  - Journal of Geosciences
VL  - 66
IS  - 4
SP  - 243-262
EP  - 243-262
PB  - Czech Geological Society
SN  - 18026222
KW  - Bohemian Massif
KW  - Moldanubian Zone
KW  - Český Krumlov Unit
KW  - pyroxene
KW  - alkali amphibole
KW  - carbonatite-like marble
UR  - http://www.jgeosci.org/detail/jgeosci.336/abstract/
N2  - Amphiboles and diopside occur in several distinct mineral assemblages in banded carbonatite-like marbles from the Bližná graphite mine, Český Krumlov Unit, Moldanubian Zone. The carbonatite-like marble is interlayered with dominant ordinary metacarbonates as a single continuous stratabound layer, up to 3-4 m thick. It is enriched in elements typical for carbonatites (REE, Y, Th, Sr, Nb, Zr, and Mo) and contains accessory betafite-pyrochlore and uranothorite along with molybdenite, sulfides (e.g., pyrite, pyrrhotite) and oxides (e.g., magnetite, ilmenite). Detailed study of thin sections in optical microscope and BSE images as well as results of EMPA revealed three distinct mineral assemblages - richterite + forsterite (RF) assemblage (Rht + Fo + Cal ˃ Dol ˃ Phl + Di), Na rich actinolite + diopside (AD) assemblage (Di + Act + Rht + Cal ˃ Phl) and magnesio-hastingsite + diopside (HD) assemblage (Mhst + Di + Cal ˃ Ab + Phl). The distinct amphibole species found within the individual assemblages exhibit complex textural relations and crystallized in several prograde and retrograde stages. The following amphibole species were recognized in the individual assemblages: RF - (richterite > ferri-winchite > tremolite, edenite), AD - (actinolite > ferri-winchite; richterite > ferri-katophorite; magnesio-riebeckite), HD - (magnesio-hastingsite; ferri-winchite, actinolite). They differ especially in Mg/(Mg + Fetot) ratio and concentrations of F. Diopside contains up to 17 mol. % of the aegirine component and albite is Fe, Ba-enriched (≥ 0.69 wt. % BaO and ≥ 0.50 wt. % Fe2O3tot). The composition of amphiboles and pyroxenes indicates the alkaline environment of their formation; unusually high Fe2O3 contents in albite plagioclase have known counterparts in alkaline pegmatites and some carbonatite dykes. The following options of potential origin of the carbonatite-like marble from Bližná are discussed: (i) metacarbonates potentially with Na- and Na,Ca-carbonates and sulfate admixture; (ii) admixture of alkaline volcanodetritic component during carbonate sedimentation; (iii) metamorphosed carbonatites enclosed in ordinary sedimentary metacarbonate; (iv) Na-rich metasomatites characterized by mineral assemblages with Na,Fe,F-enriched amphiboles, diopside with high aegirine component and albite. With regard to the observed mineral assemblages, textures and composition of minerals, we can exclude (i) marine evaporates, whereas the other options (ii), (iii) and (iv) are, in general, possible. The amphiboles observed in the Bližná carbonatite-like marble are unique within the Bohemian Massif and distinctly different from amphiboles found in metacarbonates with evaporite component.
ER  -

RADKOVÁ, Pavlína; Milan NOVÁK; Jan CEMPÍREK; Stanislav HOUZAR a Radek ŠKODA. Amphibole and pyroxene as indicators of alkaline conditions in banded carbonatite-like marbles from Bližná, Český Krumlov Unit, Moldanubian Zone. \textit{Journal of Geosciences}. Czech Geological Society, 2021, roč.~66, č.~4, s.~243-262. ISSN~1802-6222. Dostupné z: https://doi.org/10.3190/jgeosci.336.

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