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Bioclimatological background and agricultural human settlements in Monsoon Asia in Climate and agricultural land use in Monsoon Asia.
  • Bioclimatological background and agricultural human settlements in Monsoon Asia in Climate and agricultural land use in Monsoon Asia.
Evoljucija rel'efa dna okeanov atlanticeskogo tipa i ee matematiceskaja model' Evolution du relief du fond des océans de type atlantique - modèle mathématique
  • The ocean floor spreading and the subsidence of cooling oceanic plate, the transport and settling down of terrigenous sediments, the transport along the continental slope, consolidation and isostatic subsidence of sedimentary layers are considered
Model for submarine glacial deposition
  • depth), with sedimentation rates probably < 0,01 m/ka. The coarse grained texture of these deposits is caused by removal of finer grades in suspension during settling of ice rafted debris sediments. Overconsolidated till was deposited < 31 000 BP during
Sediment accumulation in low sedimentation, wave-dominated, glaciated inlets in Sedimentology of fjords.
  • sediment distribution model. Storm waves resuspend fine-grained sediment in water depths of tens of metres and produce near bottom turbid water zones within basins. Fine sands and silt settle out rapidly, leading to the deposition of graded beds
Late Holocene tectonic movements at Akhziv, Mediterranean coastline of northern Israel
  • . The transgressive marine sediments onlap and overlie a 2700-yr-old middle Iron Age (Phoenician) tomb, which was built on a dark clay layer, containing a middle Bronze IIB (3750 yr B.P.) settlement. In post-Roman times the coastal zone at this site, both east
Structure et dynamique des peuplements de termites tropicaux
  • , islands. Species isolation takes place through nest settlement, food selection, polymorphism, foraging and reproductive strategies. The pattern of communities structure presents a balance between trophic groups and between populations and resources
Beitrag zu den physikalischen Eigenschaften mariner Sedimente im Gebiet nordlich der Azoren. (Contribution à l'étude des propriétés des sédiments marins, au nord des Açores)
  • , longitudinal waves velocity and settlement. These make possible to determine and represent facies changes of the sediments as dependent on the morphology of the area of investigation. (HL).
Les Versants d'un cirque glaciaire des hautes Vosges: le Forlet. Une diversité de formes et d'évolution postglaciaire en relation avec le milieu végétal
  • Are made out, on the one hand, slopes with accumulations of blocks. They are bare and of several types. The vegetation cannot settle here and develops only locally, mainly starting from the top of the slope, making use of the pecularities
Late-Glacial and Postglacial sedimentation in Lake Superior based on seismic-reflection profiles
  • , acoustically transparent layer overlying a strong reflector, and (III) relatively thick sediment with internal acoustic reflectors. These profiles, in conjunction with sediment cores from the area, reveal that varved glacial-lacustrine sediment settled out
Subductions antérieures au charriage nord-sud de la croûte téthysienne: facteur de métamorphisme de séries sédimentaires et volcaniques liées aux assemblages ophiolitiques syro-turcs en schistes verts et amphibolites
  • -sedimentary series, settled during expansion. The metamorphism would occur in an intra-oceanic subduction zone. The metamorphic conditions would vary with the subduction rate, giving from a similar material deep greenschists and amphibolites for a low speed