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  • Andes ; Chile ; Geochronology ; Geological structure ; Isotope dating ; Landslide ; Mountain ; Quaternary ; Rockfall ; Seismicity ; Slope dynamics ; Tectonics
  • Most of the rockslides appear in the western Cordillera Principal and cluster along major geological structures. Variographic analyses show spatial correlation between rockslides, geological structures and shallow seismicity. A relative
  • of sediment transfer and the spatial distribution of rockslides reflect a landscape in which tectonic and geological controls on denudation are more significant than climate.
  • 2009
  • The geological relationships between Sardinia and Calabria during Alpine and Hercynian times
  • The AA. consider (without reaching any conclusions) four major open questions that bear on the original geologic relationships between Sardinia and Calabria, and that are closely interconnected : (1) Was Calabria a single terrane during post
  • 2009
  • 2009
  • [b1] Geochemical Processes and Environment Group, Geological Survey of Norway (NGU), Trondheim, Norvege
  • [b2] Quaternary Geology and Climate Group, Geological Survey of Norway (NGU), Trondheim, Norvege
  • [a1] Quaternary Geology and Climate Group, Geological Survey of Norway (NGU), Trondheim, Norvege
  • [a3] Geochemical Processes and Environment Group, Geological Survey of Norway (NGU), Trondheim, Norvege
  • Influence of macroscale and microscale surface roughness on multi-beam RADARSAT-1 data : implications for geological mapping in the Curaçá valley (Brazil)
  • Bahia ; Brazil ; Geological map ; Geological structure ; Image processing ; Lithology ; Principal components analysis ; RADARSAT-1 ; Remote sensing ; Roughness ; Semi-arid area ; Topography
  • 2009
  • have been used to study the geological, geomorphological and tectonic setting of the area. The results suggest the presence of a highly mature, almost flat Brahmaputra floodplain evolved during the recent geological past, in which palaeochannels had
  • 2009
  • 2009
  • [b1] Geological survey of Norway (NGU), Quaternary Geology and Climate Group, NO-7491, Trondheim, Norvege
  • [b3] Geological survey of Norway (NGU), Geohazards Group, NO-7491, Trondheim, Norvege
  • [a1] Quaternary Geology and Climate Group, Geological Survey of Norway (NGU), Trondheim, Norvege
  • [a3] Geochemical Processes and Environment Group, Geological Survey of Norway (NGU), Trondheim, Norvege
  • . A classification process helped to produce a morphometric map (10 classes), a morphoclimatic map (5 classes) and a geological map (15 classes). These 3 maps were combined using an overlay operation (union) to obtain the final terrain classification (419 classes
  • ), which was then applied to calculate diversity landscape indices. These indices were calculated for the whole landscape of the main Iberian geological regions, thus revealing a close relationship between some index values and the geological
  • 2009
  • Landsat TM and Quickbird images for geological mapping in the syn-rift Lower Dogali Formation (Red Sea Coast, NE Eritrea)
  • Data processing ; Eritrea ; Geological map ; LANDSAT ; Photointerpretation ; QUICKBIRD ; Red Sea ; Regional geology ; Satellite imagery ; Thematic Mapper
  • 2009
  • Correlation ; European part of Russia ; Geological structure ; Neotectonics ; Oil ; Tatarstan
  • 2009
  • 2009
  • [b1] British Geological Survey, Edinburgh, Royaume-Uni
  • of moving were mostly affected by geological structure (carbonate basis) and pre-glacial relief (karst and fluvial relief). During two phases of intensive glaciation, the surface that had been seized by glacial changes also changed. - (L'A.).
  • 2009
  • Barents Sea ; European part of Russia ; Geological deposit ; Mathematical model ; Murmansk ; Natural gas ; Ocean wave ; Statistical analysis ; Wind
  • 2009
  • soils from southeastern Nigeria on 2 major geological formations were sampled. Discussion of the results.
  • 2009
  • on the surface morphology and contemporary processes in all 5 rivers. Features associated with avulsions are active and distinct throughout the study area, and all the rivers have experienced geologically (if not historically) recent avulsions. However, no two
  • with late Quaternary and Holocene coastal and fluvial-deltaic processes accounts for the major differences. Results show that even within a region of similar environmental controls and geological history local variations in inherited morphology can result
  • 2009
  • 2009
  • [a1] Quaternary Geology and Climate Group, Geological Survey of Norway (NGU), Trondheim, Norvege
  • [a3] Geochemical Processes and Environment Group, Geological Survey of Norway (NGU), Trondheim, Norvege
  • 2009
  • [a1] Quaternary Geology and Climate Group, Geological Survey of Norway (NGU), Trondheim, Norvege
  • [a3] Geochemical Processes and Environment Group, Geological Survey of Norway (NGU), Trondheim, Norvege
  • 2009
  • [a1] Quaternary Geology and Climate Group, Geological Survey of Norway (NGU), Trondheim, Norvege
  • [a3] Geochemical Processes and Environment Group, Geological Survey of Norway (NGU), Trondheim, Norvege
  • 2009
  • [a1] Quaternary Geology and Climate Group, Geological Survey of Norway (NGU), Trondheim, Norvege
  • [a3] Geochemical Processes and Environment Group, Geological Survey of Norway (NGU), Trondheim, Norvege
  • Lake shapes and their spatial distribution are important geomorphological indicators in previously glaciated areas. Their shapes are influenced by the underlying geological structure and processes of glacial sediment deposition or erosion. Landsat
  • 2009
  • [b1] Dep. of Environmental, Geographical and Geologic Sciences, Lehman College, City Univ., New York, Etats-Unis
  • The AA. combine a range of geomorphologic techniques with available structural and geological data to decipher the neotectonics of a regionally significant Plio Quaternary Graben in southern Turkey (the Hatay Graben), where the rates and timing
  • of geological development of the eastern Mediterranean region and also for hazard prediction in the local area.
  • 2009