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Eifel Synclines

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Journal Article
Published: 01 March 2012
Journal of Paleontology (2012) 86 (2): 282-301.
...- and Paleotethys oceans (e.g., Pedder and Oliver, 1990 ). Rugose corals of the Eifel Synclines have been well studied since the early nineteenth century (see Birenheide, 1994 ). Most of the historical taxa described by Goldfuss (1826) , Frech (1886) , and Wedekind (e.g., 1924 ; including his students, e.g...
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Series: Geological Society, London, Special Publications
Published: 01 January 2007
DOI: 10.1144/SP278.8
EISBN: 9781862395268
... ). With the exception of the lowermost and uppermost samples in unit iKW, TOC, TS and HI values are conspicuously low throughout this interval. Abstract The Büdesheimer Bach borehole in the Prüm Syncline, Eifel Mountains, Germany encountered upper Frasnian and lowermost Famennian sediments including the Upper...
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Series: SEPM Special Publication
Published: 01 January 1974
DOI: 10.2110/pec.74.18.0155
EISBN: 9781565761483
... deltalike clastic deposits (Belgium, Aachen, Eifel) and in the eastern part as isolated reef complexes and shelf-margin reefs on local platform rises (Bergisches Land, Sauerland). (2) Isolated submarine volcanic rises in the internal part of the trough on submarine ophiolites (Lahn- Dill syncline...
Series: Geological Society, London, Special Publications
Published: 01 January 2016
DOI: 10.1144/SP423.4
EISBN: 9781862399556
... 2000 ; Huckriede et al. 2004 ; Salamon & Königshof 2010 ; Eckelmann et al. 2014 ). West of the river Rhine, the Eifel synclines, interpreted as part of the north–south-trending axial depression of the RSG, are the dominant structure (Fig. 2 ). In contrast to the entire RSG east...
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Journal Article
Published: 01 January 2009
Journal of Paleontology (2009) 83 (1): 45-62.
...-75460 ( Fig. 4.2 ). The holotype was discovered in the Olifant Member of the Ahbach Formation, lowermost Lower Givetian (Middle Devonian) of the abandoned “Müllertchen” quarry, S of Ahütte (Hillesheim syncline, Eifel, Rhenish Massif, Germany); UTM 50°20′05.41″N, 6°46′16.81″E. Partly preserved...
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Journal Article
Published: 01 January 2008
Bulletin de la Société Géologique de France (2008) 179 (1): 73-87.
... Devonian onset of the Ardenne-Eifel basin development, rather than a middle Ordovician Ardennian orogeny. 30 06 2007 01 12 2006 Société géologique de France Éditeur, Paris 2008 The recognition of an older tectonometamorphic event in basement inliers is often obscured by younger...
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Journal Article
Published: 01 March 2011
Journal of the Geological Society (2011) 168 (2): 407-422.
... compressional tectonic inversion of the Ardenne–Eifel sedimentary basin. Fracturing and sealing occurred in Lower Devonian siliciclastic multilayers under very low-grade metamorphic conditions in a brittle upper crust. A geometrical and microthermometric analysis of these veins has helped to constrain...
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Series: SEPM Special Publication
Published: 01 January 2002
DOI: 10.2110/pec.02.72.0181
EISBN: 9781565761940
... and the acme of coral and sponge reef biodiversity Two peaks are identified for reef distribution, a mid-Silurian (Wenlock) maximum and a Mid- to Late Devonian (Eifel-Givet-middle Frasne) maximum, with reefs spread to latitudes as high as 45 lo 60 degrees, and major barrier-platform tropical reef belts...
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Journal Article
Published: 01 April 2007
Clays and Clay Minerals (2007) 55 (2): 200-212.
...Sven Sindern; Helge Stanjek; Christoph Hilgers; Yvonne Etoundi Abstract Investigation of material from three core sections of the RWTH-1 drill-hole in the Wurm syncline of Aachen, Germany, shows mineralogical and structural evidence of intensive hydrothermal activity in the footwall of the Aachen...
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Journal Article
Published: 30 May 2016
Geological Magazine (2016) 154 (4): 707-739.
... discerned 18 microfacies ranging from a homoclinal ramp to a discontinuously rimmed shelf and then a drowning shelf. The comparison of these sedimentological results with those published for the south of the Dinant Syncline allowed us to provide an up to date model of the vertical and lateral environmental...
Image
1 , Geological overview of the Rhenish Massif showing the studied area (bol...
Published: 01 March 2012
F igure 2 1 , Geological overview of the Rhenish Massif showing the studied area (bold rectangle) (taken from Bohatý, 2009c ; modified from Korn, 2008 after Walter, 1995 ); 2 , detailed view of the Eifel Synclines with the fossil localities 1–8 (modified after Struve, 1996b ).
Series: Geological Society, London, Special Publications
Published: 01 January 2007
DOI: 10.1144/SP278.7
EISBN: 9781862395268
...) beuthi is known from a single locality in the Sötenich Syncline ( Jux & Strauch 1966 , p. 214). Fig. 4. Lithostratigraphy of the late Eifelian to basal Frasnian of the Eifel Hills and the Bergisch Gladbach Paffrath Syncline, with the stratigraphic range of Stringocephalus and species...
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TABLE 1—Simplified lithostratigraphic chart of the Mosel/Middle Rhine regio...
in > PALAIOS
Published: 01 April 2005
TABLE 1—Simplified lithostratigraphic chart of the Mosel/Middle Rhine region and adjacent areas. Stratigraphy of the Mosel Syncline and Middle Rhine region mainly after Meyer and Stets (1996), Eifel area after Lippert (1939) and Fuchs (1989), Olkenbach Syncline after Solle (1976), Siegerland area
Image
Figure  2 — 1 ,  Abbreviatocrinites nodosus  ( Sandberger and Sandberger, 1...
Published: 01 January 2009
of the crown MCZ-102980, lithographed by Schultze (1866 , pl. 2, fig. 2a). Locality: “Prüm” (W-Rhenish Massif, Eifel, Prüm syncline, Germany), stratigraphy (supposed): Junkerberg Formation (upper Middle Eifelian); 6 , Abbreviatocrinites nodosus ( Sandberger and Sandberger, 1856 ), CREF84-2 (Leunissen
Series: Geological Society, London, Special Publications
Published: 01 January 2016
DOI: 10.1144/SP423.11
EISBN: 9781862399556
... be, for example, ‘the lower Emsian in the Eifel region’, referring to the rocks of this age in the Eifel region. In an adjectival usage, ‘the lower Emsian strata/biozones/brachiopods’ mean that the strata/biozones/brachiopods are referred to the rock column of the ‘lower Emsian’. Depending on the context, i.e...
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Journal Article
Journal: PALAIOS
Published: 01 February 2016
PALAIOS (2016) 31 (2): 35-40.
.... Nyhuis C. Ausich W.I. Nardin E. Schröder S. 2012 , Coral-crinoid biocoenosis and resulting trace fossils from the Middle Devonian of the Eifel Synclines (Rhenish...
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Journal Article
Journal: PALAIOS
Published: 01 June 2017
PALAIOS (2017) 32 (6): 382-387.
... biocoenosis and resulting trace fossils from the Middle Devonian of the Eifel Synclines (Rhenish Massif, Germany) : Journal of Paleontology , v . 86 , p . 282 – 301 . Brett, C.E., 1999 , Middle Devonian Windom...
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Series: Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.179.01.15
EISBN: 9781862394278
... to the south by the Hunsrück–Taunus Boundary Fault, a steep wrench and normal fault, which has been repeatedly active since the early Late Carboniferous, that inverted the former suture zone. The Rhenish Massif is segmented by the north–south-trending Eifel Depression (Fig. 1 ), where Cenozoic and Mesozoic...
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Journal Article
Journal: PALAIOS
Published: 01 April 2005
PALAIOS (2005) 20 (2): 101-120.
...TABLE 1—Simplified lithostratigraphic chart of the Mosel/Middle Rhine region and adjacent areas. Stratigraphy of the Mosel Syncline and Middle Rhine region mainly after Meyer and Stets (1996), Eifel area after Lippert (1939) and Fuchs (1989), Olkenbach Syncline after Solle (1976), Siegerland area...
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Series: Geological Society, London, Memoirs
Published: 01 January 2006
DOI: 10.1144/GSL.MEM.2006.032.01.09
EISBN: 9781862394070
... Miocene-early Pliocene and in Pliocene-Quaternary times (Fig. 3 ; Dèzes et al . 2004 ). Extension continues to the present day along the Rhine and Ruhr grabens, whereas subsidence of the Massif Central grabens ceased during the Miocene. Within the Rhenish Massif, volcanic activity shifted to the Eifel...
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