Late Carboniferous palaeodepositional changes recorded by
inorganic proxies and REE data from the coal-bearing strata: An
example on the Czech part of the Upper Silesian Coal basin
(USCB)

J 2022

Late Carboniferous palaeodepositional changes recorded by inorganic proxies and REE data from the coal-bearing strata: An example on the Czech part of the Upper Silesian Coal basin (USCB)

VÖRÖŠ, Dominik; Eva GERŠLOVÁ; Lucie ŠIMONÍKOVÁ a Mercedes DIAZ-SOMOANO

Základní údaje

Originální název

Late Carboniferous palaeodepositional changes recorded by inorganic proxies and REE data from the coal-bearing strata: An example on the Czech part of the Upper Silesian Coal basin (USCB)

Autoři

VÖRÖŠ, Dominik; Eva GERŠLOVÁ (203 Česká republika, domácí); Lucie ŠIMONÍKOVÁ (203 Česká republika, domácí) a Mercedes DIAZ-SOMOANO

Vydání

Journal of Natural Gas Science and Engineering, Elsevier, 2022, 1875-5100

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10505 Geology

Stát vydavatele

Velká Británie a Severní Irsko

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 5.300

Kód RIV

RIV/00216224:14310/22:00127943

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.1016/j.jngse.2022.104789

UT WoS

000862880700003

EID Scopus

2-s2.0-85138773020

Klíčová slova anglicky

Inorganic proxies; REEs; Serpukhovian-Bashkirian; Depositional environment; Upper Silesian Coal basin

Štítky

rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 17. 1. 2023 15:17, Mgr. Marie Novosadová Šípková, DiS.

Anotace

V originále

In the Czech Republic, coal-bearing siliciclastic sediments have been deposited during the Serpukhovian and Bashkirian (Carboniferous). Until now, no attention has been paid to inorganic geochemical assessment of the coals and associated non-coal rocks from the mixed shallow-marine to continental sediments (Ostrava Forma-tion), and continental non-marine settings (Karvin ' a Formation). Samples were collected from a 750 m deep coal exploration borehole at the CSM Mine. The bulk parameters, total organic carbon TOC, total inorganic carbon TIC, total sulphur TS, major elements, trace elements, and REEs were measured on these samples, and their mineral associations have been investigated using microscopy combined with the principal component analysis (PCA). Common redox proxies V/Cr, U/Th, Ni/Co, Mo/U, and the ratio S/TOC have been tested on the samples to investigate their usefulness for studying anoxia. Research concludes that redox proxies such as U/Th, Ni/Co and V/Cr have been strongly influenced by the clastic input and carbonates, which it hinders for them to be reliable indicators of anoxia. On the basis of Eu anomaly and REEs distribution, the primary source of detrital elements comes from the parent rock, being governed more by physical than redox processes.

Citovat

VÖRÖŠ, Dominik; Eva GERŠLOVÁ; Lucie ŠIMONÍKOVÁ a Mercedes DIAZ-SOMOANO. Late Carboniferous palaeodepositional changes recorded by inorganic proxies and REE data from the coal-bearing strata: An example on the Czech part of the Upper Silesian Coal basin (USCB). Journal of Natural Gas Science and Engineering. Elsevier, 2022, roč. 107, November, s. 104789-104803. ISSN 1875-5100. Dostupné z: https://dx.doi.org/10.1016/j.jngse.2022.104789.

@article{2246078,
   author = {Vöröš, Dominik and Geršlová, Eva and Šimoníková, Lucie and DiazandSomoano, Mercedes},
   article_number = {November},
   doi = {http://dx.doi.org/10.1016/j.jngse.2022.104789},
   keywords = {Inorganic proxies; REEs; Serpukhovian-Bashkirian; Depositional environment; Upper Silesian Coal basin},
   language = {eng},
   issn = {1875-5100},
   journal = {Journal of Natural Gas Science and Engineering},
   title = {Late Carboniferous palaeodepositional changes recorded by inorganic proxies and REE data from the coal-bearing strata: An example on the Czech part of the Upper Silesian Coal basin (USCB)},
   url = {https://www.sciencedirect.com/science/article/pii/S1875510022003754?via%3Dihub},
   volume = {107},
   year = {2022}
}

TY  - JOUR
ID  - 2246078
AU  - Vöröš, Dominik - Geršlová, Eva - Šimoníková, Lucie - Diaz-Somoano, Mercedes
PY  - 2022
TI  - Late Carboniferous palaeodepositional changes recorded by inorganic proxies and REE data from the coal-bearing strata: An example on the Czech part of the Upper Silesian Coal basin (USCB)
JF  - Journal of Natural Gas Science and Engineering
VL  - 107
IS  - November
SP  - 104789
EP  - 104789
PB  - Elsevier
SN  - 18755100
KW  - Inorganic proxies
KW  - REEs
KW  - Serpukhovian-Bashkirian
KW  - Depositional environment
KW  - Upper Silesian Coal basin
UR  - https://www.sciencedirect.com/science/article/pii/S1875510022003754?via%3Dihub
N2  - In the Czech Republic, coal-bearing siliciclastic sediments have been deposited during the Serpukhovian and Bashkirian (Carboniferous). Until now, no attention has been paid to inorganic geochemical assessment of the coals and associated non-coal rocks from the mixed shallow-marine to continental sediments (Ostrava Forma-tion), and continental non-marine settings (Karvin ' a Formation). Samples were collected from a 750 m deep coal exploration borehole at the CSM Mine. The bulk parameters, total organic carbon TOC, total inorganic carbon TIC, total sulphur TS, major elements, trace elements, and REEs were measured on these samples, and their mineral associations have been investigated using microscopy combined with the principal component analysis (PCA). Common redox proxies V/Cr, U/Th, Ni/Co, Mo/U, and the ratio S/TOC have been tested on the samples to investigate their usefulness for studying anoxia. Research concludes that redox proxies such as U/Th, Ni/Co and V/Cr have been strongly influenced by the clastic input and carbonates, which it hinders for them to be reliable indicators of anoxia. On the basis of Eu anomaly and REEs distribution, the primary source of detrital elements comes from the parent rock, being governed more by physical than redox processes.
ER  -

VÖRÖŠ, Dominik; Eva GERŠLOVÁ; Lucie ŠIMONÍKOVÁ a Mercedes DIAZ-SOMOANO. Late Carboniferous palaeodepositional changes recorded by inorganic proxies and REE data from the coal-bearing strata: An example on the Czech part of the Upper Silesian Coal basin (USCB). \textit{Journal of Natural Gas Science and Engineering}. Elsevier, 2022, roč.~107, November, s.~104789-104803. ISSN~1875-5100. Dostupné z: https://dx.doi.org/10.1016/j.jngse.2022.104789.

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