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Showing 1 to 5 of 5 for “"isostatic uplift"”.

  1. Late Quaternary relative sea level change in the South Shetland Islands, Antarctica

    … by more gradual RSL fall as a consequence of isostatic uplift in response to regional deglaciation. In addition, regional GPS surveys of raised beaches were conducted to assess the spatial pattern of glacio-isostatic rebound following deglaciation. The centre of uplift was found to closely …

    durham Repository record for Late Quaternary relative sea level change in the South Shetland Islands, Antarctica (opens in a new tab)

  2. Late Cenozoic Exhumation in a Transpressional Setting: Fairweather Range, Alaska

    … Rapid recent sedimentation (> 1cm/yr) and glacio-isostatic uplift rates (> 3 cm/yr) in the Fairweather corridor highlight short-term vertical deformation at the eastern margin; however, the relationship between these rates and long-term deformation is less well known. New low-temperature cooling …

    vt Repository record for Late Cenozoic Exhumation in a Transpressional Setting: Fairweather Range, Alaska (opens in a new tab)

  3. Plio-Pleistocene Drainage Evolution of The Vera Basin, SE Spain

    … and sedimentary response of a basin undergoing uplift and inversion during the Plio-Pleistocene. Particular emphasis is placed on the drainage evolution during that period. Located within the Internal zone of the Betic Cordilleras, the Vera Basin is defined within a large left-lateral shear zone …

    plymouth Repository record for Plio-Pleistocene Drainage Evolution of The Vera Basin, SE Spain (opens in a new tab)

  4. Understanding Himalayan denudation at the catchment and orogen scale

    … are argued to be proportional to tectonic or isostatic uplift rates and provide valuable insight into the tectonic regimes underlying surface denudation. The use of denudation rates based on terrestrial cosmogenic nuclide (TCN) such as 10Beryllium has become a widely-used method to quantify …

    potsdam-diss Repository record for Understanding Himalayan denudation at the catchment and orogen scale (opens in a new tab)

  5. Intermontane valley fills

    … relative contribution to the present-day rock-uplift rate. For a range of different lithospheric and upper mantle-material properties, the results suggest that the long-wavelength uplift signal can be explained by glacial isostatic adjustment with a small erosional contribution and a …

    potsdam-diss Repository record for Intermontane valley fills (opens in a new tab)