Late Famennian correlation by miospores between the Refrath 1 borehole (Bergisch Gladbach-Paffrath Syncline, Germany) and the reference section of Chanxhe (Dinant Syncline, Belgium)
2005; Society for Sedimentary Geology; Issue: Lettres Linguagem: Inglês
10.4267/2042/4364
ISSN2108-5196
AutoresMaurice Streel, Christoph Hartkopf‐Fröder,
Tópico(s)Hydrocarbon exploration and reservoir analysis
ResumoThe Bergisch Gladbach-Paffrath Syncline and the Dinant Syncline are both part of the Ardennes-Rhenish Massif but are separated by some 100 km. In the Upper Devonian succession of the Bergisch Gladbach-Paffrath Syncline (The Bergisches Land), the Knoppenbissen Formation is assigned the Dasbergian (Hartkoph-Froder et alii, 2004). In this syncline the thermal alteration index (TAI of 2 to 2+) is remarkably low compared to that of other Upper Devonian sediments in the Ardenne-Rhenisch area.
Referência(s)