Burial and thermal history modelling of the Upper Carboniferous strata based on vitrinite reflectance data from Bzie-Dębina-60 borehole (Upper Silesian Coal Basin, southern Poland)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F19%3A73600292" target="_blank" >RIV/61989592:15310/19:73600292 - isvavai.cz</a>

Výsledek na webu

<a href="https://journals.muni.cz/gvms/article/view/11023" target="_blank" >https://journals.muni.cz/gvms/article/view/11023</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.5817/GVMS2019-1-2-73" target="_blank" >10.5817/GVMS2019-1-2-73</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Burial and thermal history modelling of the Upper Carboniferous strata based on vitrinite reflectance data from Bzie-Dębina-60 borehole (Upper Silesian Coal Basin, southern Poland)

Popis výsledku v původním jazyce

Integrated modeling of the coal rank in the Upper Carboniferous sediments of the Bzie-Dębina-60 borehole from SW of the Upper Silesian Coal Basin was performed based on a new vitrinite reflectance measurements from the Westphalian A. Microscopic investigations of Westphalian samples in the Bzie-Debina-60 well have shown that organic matter is dominated by vitrinite maceral group. The coal rank in the well shows an increase with depth. The mean vitrinite reflectance values in these samples range from 0.76 to 1.07 %. One-dimensional forward modelling of thermal maturity in the Bzie-Dębina-60 borehole section has been performed in order to explain the burial and thermal history. The maximum temperature (c. 145 °C) causing the coalification occurred in the Latest Carboniferous (c. 300 Ma). These processes were likely related to significant late Variscan burial heating in this area as indicated by previous authors.

Název v anglickém jazyce

Burial and thermal history modelling of the Upper Carboniferous strata based on vitrinite reflectance data from Bzie-Dębina-60 borehole (Upper Silesian Coal Basin, southern Poland)

Popis výsledku anglicky

Integrated modeling of the coal rank in the Upper Carboniferous sediments of the Bzie-Dębina-60 borehole from SW of the Upper Silesian Coal Basin was performed based on a new vitrinite reflectance measurements from the Westphalian A. Microscopic investigations of Westphalian samples in the Bzie-Debina-60 well have shown that organic matter is dominated by vitrinite maceral group. The coal rank in the well shows an increase with depth. The mean vitrinite reflectance values in these samples range from 0.76 to 1.07 %. One-dimensional forward modelling of thermal maturity in the Bzie-Dębina-60 borehole section has been performed in order to explain the burial and thermal history. The maximum temperature (c. 145 °C) causing the coalification occurred in the Latest Carboniferous (c. 300 Ma). These processes were likely related to significant late Variscan burial heating in this area as indicated by previous authors.

Druh

J_SC - Článek v periodiku v databázi SCOPUS

CEP obor

—

OECD FORD obor

10505 - Geology

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2019

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Geological Research in Moravia and Silesia

ISSN

1212-6209

e-ISSN

—

Svazek periodika

26

Číslo periodika v rámci svazku

1-2

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

7

Strana od-do

73-79

Kód UT WoS článku

—

EID výsledku v databázi Scopus

2-s2.0-85079242129