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Congress report: Geomorphology in Paris. The 26th International Geological Congress, 7-17 July, 1980
  • Congress report: Geomorphology in Paris. The 26th International Geological Congress, 7-17 July, 1980
  • Ancien rivage ; Congrès géologique international, 26, Paris, 1980 ; Géographie physique ; Géomorphogenèse ; Néotectonique ; Paléoclimatologie ; Quaternaire ; Quaternaire marin
  • 1980
Observations of flexure and the geological evolution of the Pacific Ocean basin
  • Observations of flexure and the geological evolution of the Pacific Ocean basin
  • on the continents, is one of the largest to be documented in the geological record.
  • 1980
Man as a geological agent: the sea-cliffs of Llantwit Major, Wales in Coasts under stress.
  • Man as a geological agent: the sea-cliffs of Llantwit Major, Wales in Coasts under stress.
  • 1980
Geological observations from a submersible dive on the western continental slope of the armorican massif
  • Geological observations from a submersible dive on the western continental slope of the armorican massif
  • 1980
The Jan Mayen Ridge synthesis of geological knowledge and new data
  • The Jan Mayen Ridge synthesis of geological knowledge and new data
  • 1980
Preliminary results of a seismic refraction study in the Meriadzek-Trevelyan area, Bay of Biscay
  • Four main geological sequences have been established: Cenozoic (1.9 to 2.8km/s)| Cretaceous (3.2 to 4.0km/s)| lower to middle Mesozoic (4.5 to 5.0km/s)| pre-Mesozoic (5.4 to 6.3km/s). These agree broadly with the adjoining western approaches
  • 1980
Interpretation of the Lateglacial marine environment of NW Europe by means of foraminiferida in Studies in the Lateglacial of North-West Europe.
  • The Lateglacial is in geological terms very short and in absolute chronology closely defined. Within north-west Europe planktonic foraminifera are rare or absent and study is consequently confined to bottom-dwelling species. As these species
  • 1980
Postglacial diatom stratigraphy of Kirchner Marsh, Minnesota
  • , Geological Society of America Bulletin 77, 1339-1360) show that this shift to shallow-water diatoms occurred when aquatic macrophytes appeared at the site in abundance.
  • 1980
Etude de l'effet de marée océanique sur un aquifère carbonaté côtier (Miocène de l'Algarve-Portugal)
  • general hydrodynamical behaviour. The model that gives the most satisfying reconstitutions of the observations points out a seepage situation which fits quite well to the known geological conditions of the aquifer. (The AA).
  • 1980
Wastage of the Klutlan ice-cored moraines, Yukon Territory, Canada
  • of ice with a debris concentration of 1%, or about 1200 yr for a 1.5% debris load. Another meltout curve, based on seismic data, suggests total meltout in about 875 yr. When all geologic factors are considered, the empirical meltout curve is remarkably
  • 1980
New evidence from beneath the western North Atlantic for the depth of glacial erosion in Greenland and North America
  • account for the remainder. The documented erosion in part substantiates W. A. White's (1972, Geological Society of America Bulletin 83, 1037-1056) hypothesis of deep erosion and exhumation of shield regions, but is not in agreement with the entire volume
  • 1980