Organic maturation levels and thermal history of the Carboniferous rocks of the Dublin Basin

Fernandes, Paulo; Clayton, Geoff

http://hdl.handle.net/10400.1/5117

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Authors

Fernandes, Paulo

Clayton, Geoff

Abstract(s)

The Dublin Basin sucession comprises sediments in age from Mississippian (Courceyan) to Pennsylvanian (Langsettian). The Viséan part of. the succession is dominated by turbiditic calcarenites interbedded with grey-black shales. Namurian and earliest Westphalian rocks preserved in the Kingscourt Outlier in the north of the basin are dominated by sandstones interbedded with silstones and shales.

Keywords

Dublin Basin Ireland Maturation levels Thermal history

URI

http://hdl.handle.net/10400.1/5117

Citation

Fernandes, Paulo; Clayton, Geoff. Organic maturation levels and thermal history of the Carboniferous rocks of the Dublin Basin, Trabalho apresentado em XVth International Congress on Carboniferous and Permian Stratigraphy, In Proceedings of the XVth International Congress on Carboniferous and Permian Stratigraphy, Royal Netherlands Academy of Arts and Sciences, Utrecht, 2007.