Geologica Belgica

1374-8505 2034-1954

 

Facteur d'impact : 1.8 (2022)

depuis le 05 février 2011 :
Visualisation(s): 406 (1 ULiège)
Téléchargement(s): 687 (0 ULiège)
print        
Krystian PROBIERZ & Małgorzata LEWANDOWSKA

PALEOTEMPERATURES OF UPPER CARBONIFEROUS SEDIMENTARY ROCKS IN THE NW PART OF THE UPPER SILESIAN COAL BASIN, POLAND

(volume 7 (2004) — number 3-4 - Proceedings of the 5th European Coal Conference)
Article
Open Access

Document(s) associé(s)

Annexes

Mots-clés : Upper Silesian Coal Basin, Carboniferous sedimentary rocks, paleotemperature, paleothermal gradient

Abstract

Paleothermal conditions of Upper Carboniferous sedimentary rocks in the strongly folded north-westernpart of the Upper Silesian Coal Basin (USCB) are characterized in this paper. NS-oriented narrow folds predominate, with amplitudes ranging from 100 to 800 m, often dislocated by axial faults. The paleothermal conditions, i.e. maximum paleotemperatures and paleothermal gradient were calculated according to Bostick’s nomogram and Barker and Pawlewicz’s method on the basis of studies of 115 samples of coal taken from depths between +17 and -368 m b.s.l. The paleotemperatures range from 135 to 220oC and the paleothermal gradients from 2.4 to 5.9oC/100 m. The coalification process probably has a synorogenic character.

Pour citer cet article

Krystian PROBIERZ & Małgorzata LEWANDOWSKA, «PALEOTEMPERATURES OF UPPER CARBONIFEROUS SEDIMENTARY ROCKS IN THE NW PART OF THE UPPER SILESIAN COAL BASIN, POLAND», Geologica Belgica [En ligne], number 3-4 - Proceedings of the 5th European Coal Conference, volume 7 (2004), 313-318 URL : https://popups.uliege.be/1374-8505/index.php?id=432.

A propos de : Krystian PROBIERZ

Silesian University of Technology, Faculty of Mining and Geology, Institute of Applied Geology, Akademicka 2, 44-100 Gliwice. E-mail : probierz@zeus.polsl.gliwice.pl

A propos de : Małgorzata LEWANDOWSKA

Silesian University of Technology, Faculty of Mining and Geology, Institute of Applied Geology, Akademicka 2, 44-100 Gliwice.