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Par Collection Par Auteur Par Date Par Sujet Par Titre
  • Armenia ; Caucasus ; Earthquake ; Geological map ; Geological structure ; Landform evolution ; Neotectonics
  • 2013
  • 2013
  • [b1] Western Geographic Science Center, United States Dept. of the Interior, United States Geological Survey, Menlo Park, CA, Etats-Unis
  • [b2] Western Ecological Research Center, Las vegas Field Station, United States Dept. of the Interior,United States Geological Survey, NV, Henderson, Etats-Unis
  • [b3] Geology, Energy, Minerals, and Geophysics Science Center, United States Dept. of the Interior, United States Geological Survey, Menlo Park, CA, Etats-Unis
  • [b4] Western Remote Sensing and Visualization Center, United States Dept. of the Interior, United States Geological Survey, CA, Sacramento, Etats-Unis
  • 2013
  • [b2] U.S. Geological Survey, Illinois Water Science Center, Urbana, Etats-Unis
  • [b3] U.S. Geological Survey, Washington Water Science Center, Tacoma, Etats-Unis
  • [b5] U.S. Geological Survey, Office of Surface Water, Urbana, Etats-Unis
  • [b7] U.S. Geological Survey, Office of Surface Water, Louisville, Etats-Unis
  • 2013
  • [b1] Dept. of Research and Geoscientific Prospective, Geological Survey of Spain (IGME), Madrid, Espagne
  • [b2] Mining and Geological Engineering Dep., Univ. Castilla-La Mancha, Toledo, Espagne
  • [b3] Lab. of Dendrogeomorphology, Inst. of Geological Sciences, Univ., Berne, Suisse
  • -Geoengineering knowledge: interdisciplinarity and the shaping of climate engineering research ; 4-Geoengineering and geologic politics.
  • 2013
  • Morphological evidence for geologically young thaw of ice on Mars : A review of recent studies using high-resolution imaging data
  • 2013
  • 2013
  • [b1] Dep. of Research and Geoscientific Prospective, Geological Survey of Spain (IGME), Madrid, Espagne
  • [b2] Mining and Geological Engineering Dep., Univ. Castilla-La Mancha, Toledo, Espagne
  • 2013
  • [b1] Dep. of Geological Engineering, Univ., Mersin, Turquie
  • [b2] Osmangazi Univ., Dep. of Geological Engineering, Eskisehir, Turquie
  • 2013
  • [b1] Michigan Technological Univ., Dept. of Geological and Mining Engineering and Sciences, Houghton, Etats-Unis
  • [b2] Dept. of Geological Sciences, Univ. of Florida, Gainesville, Etats-Unis
  • 2013
  • [b1] Dept. of Geological and Mining Engineering and Sciences, Houghton, Etats-Unis
  • [b2] Dept. of Geological Sciences, Univ. of Florida, Gainesville, Etats-Unis
  • evidence for abrasion, the AA. explore conditions in the geological past for tides that may have locally eroded bedrock.
  • 2013
  • [b4] Geological Survey of Canada (Atlantic), Natural resources, Dartmouth, Canada
  • Carrying capacity ; Fluvial erosion ; Geological structure ; Knickpoint ; Lithology ; Longitudinal section ; Sediment load ; Stream ; Taiwan
  • . Knickpoint propagation was influenced by geological structure, lithology, and drainage organization. In particular, a change in dip of the sandstone beds at the site caused a decrease of knickpoint propagation velocity.
  • 2013
  • 2013
  • [b1] US Geological Survey, Reston, Etats-Unis
  • [b2] US Geological Survey, Baltimore, Etats-Unis
  • The lower alluvial Pineios River has reacted to major geological controls, surface deformation and uplift movements caused by the activity of the recently mapped Pineios normal fault zone and salt tectonics in Kyllini peninsula resulting
  • in the river flow diversion from north to south at completely different open sea areas. The effects of the geological, tectonic and neotectonic activity and the impact of the human presence and influence on the lower Pineios River are presented in this paper
  • 2013
  • In the Szokolya Basin we can recognize a special type of recent travertine deposition, which can be explained by the geologic, geomorphologic and hidrologic conditions of the research area (measurement of water hardness, drillings, XRD, measurement
  • 2013
  • 2013
  • [b2] Inst. of Geological Sciences, Dept. of Hydrogeology, Univ., Wrocław, Pologne
  • 2013
  • [b3] Dep. of Geological Engineering, Univ., Aksaray, Turquie
  • European part of Russia ; Geological structure ; Palaeosol ; Pedogenesis ; Pedostratigraphy ; Pleistocene ; Russian Plain ; Sedimentary rock ; Stratigraphical horizon
  • 2013
  • 2013
  • [b2] External Geodynamics and Hydrogeology Group, Dept. of Geology, Geological Cabinet of Territorial and Environmental Analysis (GATA), Autonomous Univ., Barcelona, Espagne
  • [b3] Geological Survey of Ireland, Dublin, Irlande
  • 2013
  • [b4] U.S. Geological Survey, Boulder, Etats-Unis
  • [b5] U.S. Geological Survey, Menlo Park, Etats-Unis