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  • . The A. investigates the area where the density of dolines is highest and investigates the relationships between doline occurrence and geological/geomorphological conditions.
  • 1997
  • and geological sites ranging in age from the late Pleistocene through the early Holocene. They therefore suggest that hackberry endocarp is a suitable substrate for C 14 dating provided that its morphological and mineralogical integrity is preserved.
  • 1997
  • 1997
  • [b1] Illinois State Geological Survey, Champaign, Etats-Unis
  • 1997
  • [b1] US Geological Survey, Reston, Etats-Unis
  • Low-temperature thermochronology, such as that provided by apatite fission-track analysis, provides a valuable means of establishing the timing of major denudational events and associated rates of denudation over geological time-scales of 106-108 Ma
  • 1997
  • 1997
  • [b1] Dept. of Geological Sciences, Rutgers University, New Brunswick, Etats-Unis
  • 1997
  • [b1] U.S. Geological Survey, Federal Center, Denver, Etats-Unis
  • 1997
  • [b1] Dep. Geological Sciences, Univ. Illinois, Chicago, Etats-Unis
  • 1997
  • [b1] Dep. Geological Sciences, Univ. Saskatchewan, Saskatoon, Canada
  • 1997
  • [b1] Illinois State Geological Survey, Champaign, Etats-Unis
  • Aerial photography ; Canada ; Fault ; Geological structure ; Geophysics ; Glacial features ; Moraine ; Photointerpretation ; Quaternary ; Saskatchewan ; Shear stress ; Stratigraphy
  • 1997
  • Asian part of Russia ; Folding ; Geological structure ; Geomorphogenesis ; Geomorphology ; Krasnodar ; Neotectonics ; Regional geology ; Ukraine
  • 1997
  • Geological structure ; Geomorphogenesis ; Geophysics ; Global tectonics ; Island arc ; Neotectonics ; Pacific Region ; Plate tectonics ; Regional geology ; Structural geomorphology
  • 1997
  • Both aquatic and land snails are common in the geologic record, but their utility in dating is greatly resticted by their well-documented tendency to yield C 14 dates inconsistent with true C 14 ages. In this study, the AA. examine the use of C 14
  • 1997
  • 1997
  • [b1] U.S. Geological Survey, Federal Center, Denver, Etats-Unis