Results 101 to 110 of about 160 (139)
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Meta Alkali Basaltic Volcanics do Occur in the Palaeozoic of the Rhenish Mountains
1987A spilitic dolerite sill is described from Wasenbach valley at the southwestern end of the Lahn syncline in the southern Rhenish Mountains. The emplacement of the sill was guided by a smaller previously intruded sill which forms together with its contact zone the roof of the larger intrusion.
H. D. Nesbor, H. Flick
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Presence of land-plants on a volcanic island in a Devonian Sea (Rhenish Mountains, West Germany)
Review of Palaeobotany and Palynology, 1988Abstract Remains of land-plants have been found in parautochthonous position in volcaniclastic sediments of the Middle Devonian of the Lahn syncline (Rhenish Mountains). These sediments resulted from the interaction of volcanic activity, littoral erosion and reef building.
Heiner Flick +2 more
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Zeitschrift der Deutschen Gesellschaft für Geowissenschaften, 2015
The isochronous, mid-Brigantian (latest Visean) Actinopteria Black Shale is intercalated in between upper Visean calciturbidites within the northern part of the Rhenish Mountains (Germany). It shows characteristic mass-occurrences of the eponymous bivalve Ptychopteria (Actinopteria) lepida (Goldfuss).
Christian J. Nyhuis +2 more
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The isochronous, mid-Brigantian (latest Visean) Actinopteria Black Shale is intercalated in between upper Visean calciturbidites within the northern part of the Rhenish Mountains (Germany). It shows characteristic mass-occurrences of the eponymous bivalve Ptychopteria (Actinopteria) lepida (Goldfuss).
Christian J. Nyhuis +2 more
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2011
The ammonoids from the middle Famennian black limestone nodules at Kattensiepen (Rhenish Mountains) are known for their excellent preservation and show frequent sublethal shell damage of varying dimensions and of the finest detail. 76% of all specimens show traces of predation.
Slotta, F +4 more
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The ammonoids from the middle Famennian black limestone nodules at Kattensiepen (Rhenish Mountains) are known for their excellent preservation and show frequent sublethal shell damage of varying dimensions and of the finest detail. 76% of all specimens show traces of predation.
Slotta, F +4 more
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Palaeogeography of the Rhenish Slate Mountain region during the Early Devonian
Zeitschrift der Deutschen Gesellschaft für Geowissenschaften, 2021Edouard Grigowski, Tom McCann
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Geological Journal, 2008
AbstractThe Viséan (Carboniferous) sedimentary succession of the basinal Kulm facies (Rhenish Mountains) was investigated in detail in order to achieve a high‐resolution stratigraphic subdivision and correlation. Additionally, the ranges of fossil index taxa (ammonoids), fossil marker beds, volcaniclastic horizons and sedimentary features (e.g.
Dieter Korn, Bernd Kaufmann
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AbstractThe Viséan (Carboniferous) sedimentary succession of the basinal Kulm facies (Rhenish Mountains) was investigated in detail in order to achieve a high‐resolution stratigraphic subdivision and correlation. Additionally, the ranges of fossil index taxa (ammonoids), fossil marker beds, volcaniclastic horizons and sedimentary features (e.g.
Dieter Korn, Bernd Kaufmann
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1987
A reconnaissance prospection for base metal and barite mineralizations in the left Rhenish Slate Mountains by the Bundesanstalt fur Geowissenschaften and Rohstoffe, Hannover, in 1973–1977 has identified a large number of promising areas, so that follow-up investigations were carried out within the scope of a research project of the Ministry of ...
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A reconnaissance prospection for base metal and barite mineralizations in the left Rhenish Slate Mountains by the Bundesanstalt fur Geowissenschaften and Rohstoffe, Hannover, in 1973–1977 has identified a large number of promising areas, so that follow-up investigations were carried out within the scope of a research project of the Ministry of ...
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The Holocene, 2011
The distribution, thickness and composition of the floodplain sediments in the valleys of the Gelbach (Lower Westerwald) and Große Nister (Upper Westerwald) depend on the occurrence of loessic periglacial cover beds in their catchments as well as on historical land use.
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The distribution, thickness and composition of the floodplain sediments in the valleys of the Gelbach (Lower Westerwald) and Große Nister (Upper Westerwald) depend on the occurrence of loessic periglacial cover beds in their catchments as well as on historical land use.
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1983
Since the Oligocene, the Hunsriick was uplifted about 200–250 m, in relation to the Rheinhessen Plateau (Mayence Basin), and tilted southwards with amounts of up to 50 m. The plateau uplift includes parts of the Saar-Nahe Basin. The quaternary partial uplift does not exceed 40–50 m.
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Since the Oligocene, the Hunsriick was uplifted about 200–250 m, in relation to the Rheinhessen Plateau (Mayence Basin), and tilted southwards with amounts of up to 50 m. The plateau uplift includes parts of the Saar-Nahe Basin. The quaternary partial uplift does not exceed 40–50 m.
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Field trip E7: Selected Geosites in the northern Rhenish Mountains
Schriftenreihe der Deutschen Gesellschaft für Geowissenschaften, 2010M. Piecha, K.-H. Ribbert
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