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PORTAIL D'INFORMATION GÉOGRAPHIQUE

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  • An outline of the geological structure of the Northeastern Hohes Venn Area and of its Northern foreland
  • Lower Paleozoic (Cambrian, Ordovician), Devonian, and Carboniferous sedimentary rocks are exposed in the northeastern part of the Hohes Venn area (Northern Eifel) and in its northern forelands. The regional geological development represented
  • by these sediments and their Caledonian and Variscan structural characteristics are obtained from geological profiles across the Eifel's northern boundary zone.
  • 1985
  • Geological models for the configuration, history and style of disintegration of the Laurentide ice sheet in Models in geomorphology.
  • Presents models derived from current glacial geological information on three aspects of the Laurentide ice sheet : its configuration and centers of outflow| the latter part of its history of waxing and Waning and the style of its final deterioration
  • 1985
  • Simulation of the climate of 18,000 years BP : results for the North America/North Atlantic/European sector and comparison with the geologic record of North America
  • temperature were prescribed from CLIMAP (1981). The geologic evidence is generally compatible with the model simulation.
  • 1985
  • A morahalmi Madarasz-to foldtani és vizfoldtani viszonyai. (The geological and hydrogeological conditions of Lake Madarasz near Morahalom)
  • 1985
  • The economic geological importance of the lignite at the foreland of the Northern Hungarian Uplands in Problems of the Neogene and Quaternary in the Carpathian Basin.
  • 1985
  • Philosophie und Geologie. Beiträge zum III. DDR-UdSSR-Symposium zur Geschichte der geologischen Wissenschaften.. (Philosophy and geology. Papers of the third GDR-USSR-Symposium on History of geological sciences)
  • 1985
  • Carte géologique internationale de l'Afrique = International geological map of Africa. Feuille 3.
  • 1985
  • Radiocarbon dates from the East China Sea and their geological implications
  • 1985
  • Toelichting bij de Geologische kaart van Nederland 1: 50 000. Blad Eindhoven West (51 W).. (Explanation to the Geological map of the Netherlands 1: 50 000. Sheet Eindhoven West (51 W)
  • 1985
  • Based on a joint analysis of molluscs, ostracods and mammals as well as available geological and paleogeographical information, an attempt was made to correlate the Pannonian sediments with those of Eastern and Mediterranean. DLO).
  • 1985
  • A volume for the 8th Congress of the Regional Committee on Mediterranean Neogene stratigraphy, Budapest, September 1985. The study of the conditions and rate of deposition of the several thousand metres of Neogene and Quaternary sediments
  • in the Great Hungarian Plain and the denudation chronology of the Hungarian Mountains are studied with the application of geological, sedimentological, stratigraphical, paleontological and geomorphological methods and various absolute dating techniques. DLO).
  • 1985
  • The well known Clovis and Plainview paleo-indian sites of New Mexico and Texas have yielded new data on regional late Quaternary geologic, paleoclimatic, and pedologic histories.
  • 1985
  • A correlation is analysed between strength characteristics of solid rocks and selective weathering processes, field observation data being used from an alpine area in Central Tien-Shan. Geological and geomorphological survey revealed coincidence
  • 1985
  • especially alluded to the possible increase of the geological and economical availability of raw material.
  • 1985
  • An essential supposition for the effective utilization of deposits is their geologic-ecological valuation. Four groups of deposits with different value, quantity and quality are distinguished. The territorial effects of the historical location
  • 1985
  • Geological and palynological investigations of two main dune systems west of Nieuwpoort. The Old Dune system is believed to be older than 4300 B.P. The Young Dune area has a complex history: older dunes (2800-900 B.P.) underneath the Young Dune
  • 1985
  • South of Budapest, the Danube formed a loess bluff of 30 to 50 m height along 180 km length, where landslides are frequent. Observations underline the role of infiltration above the impervious layer and the reduction of spring activity. Geological
  • 1985
  • The question of whether a possible landbridge (s) existed between Britain and Ireland during Devensian (Midlandian) Late-glacial and Holocene time is analysed in the light of new geological and related environmental information. If any landbridge
  • 1985
  • Since 1973 geologists from the GDR have been involved in geologic activities in Antarctica included in the SCAR program. As participants of Soviet Antarctic expeditions they have generally dealt with problems of structural geology in selected
  • 1985
  • The results of fortnightly baseflow quality analyses of a small urban catchment are reported. It is shown that the geological formations in the catchment, consisting mainly of Table Mountain Sandstone, have a limited effect on the water quality
  • 1985