Heat flow evolution, subsidence and erosion in Upper Silesian
Coal Basin, Czech Republic

J 2016

Heat flow evolution, subsidence and erosion in Upper Silesian Coal Basin, Czech Republic

GERŠLOVÁ, Eva, Marek GOLDBACH, Milan GERŠL a Petr SKUPIEN

Základní údaje

Originální název

Heat flow evolution, subsidence and erosion in Upper Silesian Coal Basin, Czech Republic

Autoři

GERŠLOVÁ, Eva (203 Česká republika, garant, domácí), Marek GOLDBACH (203 Česká republika, domácí), Milan GERŠL (203 Česká republika) a Petr SKUPIEN (203 Česká republika)

Vydání

International Journal of Coal Geology, 2016, 0166-5162

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Nizozemské království

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 4.783

Kód RIV

RIV/00216224:14310/16:00089598

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.1016/j.coal.2015.12.007

UT WoS

000371554300003

Klíčová slova anglicky

thermal maturity;vitrinite reflectance;RE pyrolysis;Upper Silesian Coal Basin;1D basin modelling;

Štítky

AKR

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 20. 9. 2018 19:31, doc. Mgr. Eva Geršlová, Ph.D.

Anotace

V originále

The deep boreholes in the Upper Silesian Coal Basin provide a valuable material to evaluate thermal maturity of the present Carboniferous units. 17 boreholes were used for evaluating expected paleothicknesses of the missing units and the maximum temperatures reached via 1D modelling. The models consider the geological evolution concepts accepted for the region. The reliability of the final thermal models was calibrated with vitrinite reflectance data. Vitrinite reflectance varies between 0.46 and 2.32 %Rr indicating thermally early mature to over mature organic matter for the Ostrava Fm. and Karviná Fm. The coal rank increases from the east to the west. Based on the data from RockEval pyrolysis all samples from the Ostrava and Karviná Fm. belong to type III kerogen. The RE results show that the source potential of the Carboniferous sediments was not spent in full as part of the Variscan tectogen. Burial and thermal history on the Czech side of the Upper Silesian Coal Basin was reconstructed. The set of several 1D simulations proved that the thickness of the missing Palaeozoic Molasses association is 2,500 to 3,400 m in the foreland and 1,800 to 2,000 m for the platform. The maximum burial is expected at the end of the Westphalian. The consequent sedimentation of the Carpathian Foredeep and nappe thrusting did not change the Palaeozoic thermal maturity pattern within the tested area of the USCB.

Návaznosti

MUNI/M/0081/2013, interní kód MU

Název: Energetická infrastruktura a její vliv na energetickou bezpečnost

Investor: Masarykova univerzita, Energetická infrastruktura a její vliv na energetickou bezpečnost, INTERDISCIPLINARY - Mezioborové výzkumné projekty

Citovat

GERŠLOVÁ, Eva, Marek GOLDBACH, Milan GERŠL a Petr SKUPIEN. Heat flow evolution, subsidence and erosion in Upper Silesian Coal Basin, Czech Republic. International Journal of Coal Geology. 2016, roč. 154, January, s. 30-42. ISSN 0166-5162. Dostupné z: https://dx.doi.org/10.1016/j.coal.2015.12.007.

@article{1340768,
   author = {Geršlová, Eva and Goldbach, Marek and Geršl, Milan and Skupien, Petr},
   article_number = {January},
   doi = {http://dx.doi.org/10.1016/j.coal.2015.12.007},
   keywords = {thermal maturity;vitrinite reflectance;RE pyrolysis;Upper Silesian Coal Basin;1D basin modelling;},
   language = {eng},
   issn = {0166-5162},
   journal = {International Journal of Coal Geology},
   title = {Heat flow evolution, subsidence and erosion in Upper Silesian Coal Basin, Czech Republic},
   url = {http://www.elsevier.com/locate/ijcoalgeo},
   volume = {154},
   year = {2016}
}

TY  - JOUR
ID  - 1340768
AU  - Geršlová, Eva - Goldbach, Marek - Geršl, Milan - Skupien, Petr
PY  - 2016
TI  - Heat flow evolution, subsidence and erosion in Upper Silesian Coal Basin, Czech Republic
JF  - International Journal of Coal Geology
VL  - 154
IS  - January
SP  - 30-42
EP  - 30-42
SN  - 01665162
KW  - thermal maturity;vitrinite reflectance;RE pyrolysis;Upper Silesian Coal Basin;1D basin modelling;
UR  - http://www.elsevier.com/locate/ijcoalgeo
L2  - http://www.elsevier.com/locate/ijcoalgeo
N2  - The deep boreholes in the Upper Silesian Coal Basin provide a valuable material to evaluate thermal maturity of the present Carboniferous units. 17 boreholes were used for evaluating expected paleothicknesses of the missing units and the maximum temperatures reached via 1D modelling. The models consider the geological evolution concepts accepted for the region. The reliability of the final thermal models was calibrated with vitrinite reflectance data. Vitrinite reflectance varies between 0.46 and 2.32 %Rr indicating thermally early mature to over mature organic matter for the Ostrava Fm. and Karviná Fm. The coal rank increases from the east to the west. Based on the data from RockEval pyrolysis all samples from the Ostrava and Karviná Fm. belong to type III kerogen. The RE results show that the source potential of the Carboniferous sediments was not spent in full as part of the Variscan tectogen. Burial and thermal history on the Czech side of the Upper Silesian Coal Basin was reconstructed. The set of several 1D simulations proved that the thickness of the missing Palaeozoic Molasses association is 2,500 to 3,400 m in the foreland and 1,800 to 2,000 m for the platform. The maximum burial is expected at the end of the Westphalian. The consequent sedimentation of the Carpathian Foredeep and nappe thrusting did not change the Palaeozoic thermal maturity pattern within the tested area of the USCB.
ER  -

GERŠLOVÁ, Eva, Marek GOLDBACH, Milan GERŠL a Petr SKUPIEN. Heat flow evolution, subsidence and erosion in Upper Silesian Coal Basin, Czech Republic. \textit{International Journal of Coal Geology}. 2016, roč.~154, January, s.~30-42. ISSN~0166-5162. Dostupné z: https://dx.doi.org/10.1016/j.coal.2015.12.007.

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