Late Famennian correlation by miospores between the Refrath 1 borehole (Bergisch Gladbach-Paffrath Syncline, Germany) and the reference section of Chanxhe (Dinant Syncline, Belgium)
The 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-Fröder 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.
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Dokumenttyp: | Artikel |
Erscheinungsdatum: | 2005 |
Reihe/Periodikum: | Carnets de Géologie, Vol CG2005, p M02_Abstract10 (2005) |
Verlag/Hrsg.: |
Association Carnets de Geologie
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Schlagwörter: | Famennian / miospores / Germany / Belgium / biostratigraphy / Geology / QE1-996.5 / Paleontology / QE701-760 / Stratigraphy / QE640-699 |
Sprache: | Englisch Französisch |
Permalink: | https://search.fid-benelux.de/Record/base-28532055 |
Datenquelle: | BASE; Originalkatalog |
Powered By: | BASE |
Link(s) : | https://doaj.org/article/8fc36d0860894f2dbee8f935ec92f0ad |