Results 151 to 160 of about 229,083 (186)
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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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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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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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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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Geoderma, 2008
Abstract The spatial extent of metal contamination caused by small-scale ore veins is increased by periglacial solifluction. Our objectives were (1) to examine the spatial distribution of Pb in cover beds that migrated over Pb ore veins, (2) to calculate the transport distance of ore-derived Pb, and (3) to determine controls on the transport distance.
Stefan Stückrad +2 more
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Abstract The spatial extent of metal contamination caused by small-scale ore veins is increased by periglacial solifluction. Our objectives were (1) to examine the spatial distribution of Pb in cover beds that migrated over Pb ore veins, (2) to calculate the transport distance of ore-derived Pb, and (3) to determine controls on the transport distance.
Stefan Stückrad +2 more
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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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Upper Frasnian ammonoids (Tornoceratidae) from Büdesheim (Eifel Mountains, Rhenish Massif, Germany)
Palaeontographica Abteilung A, 2023Till Söte, Ralph Thomas Becker
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Late Givetian ammonoids from Iserlohn and Neuenrade (northern Rhenish Mountains)
Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen, 2017Jürgen Bockwinkel, Dieter Korn
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