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      GLOBAL GLACIAL ISOSTASY AND THE SURFACE OF THE ICE-AGE EARTH: The ICE-5G (VM2) Model and GRACE

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      Journal: Annual Review of Earth and Planetary Sciences
      Publisher: Annual Reviews

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          Calibration of the 14C timescale over the past 30,000 years using mass spectrometric U–Th ages from Barbados corals

          Edouard Bard, Bruno Hamelin, Richard Fairbanks … (1990)
          Article 0 comments Cited 492 times – based on 0 reviews     Review now
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            Rheology of the upper mantle: a synthesis.

            S Karato, P Wu (1993)
            Rheological properties of the upper mantle of the Earth play an important role in the dynamics of the lithosphere and asthenosphere. However, such fundamental issues as the dominant mechanisms of flow have not been well resolved. A synthesis of laboratory studies and geophysical and geological observations shows that transitions between diffusion and dislocation creep likely occur in the Earth's upper mantle. The hot and shallow upper mantle flows by dislocation creep, whereas cold and shallow or deep upper mantle may flow by diffusion creep. When the stress increases, grain size is reduced and the upper mantle near the transition between these two regimes is weakened. Consequently, deformation is localized and the upper mantle is decoupled mechanically near these depths.
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              Deformation of the Earth by surface loads

              W Farrell (1972)
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                Author and article information

                Journal
                Title: Annual Review of Earth and Planetary Sciences
                Abbreviated Title: Annu. Rev. Earth Planet. Sci.
                Publisher: Annual Reviews
                ISSN (Print): 0084-6597
                ISSN (Electronic): 1545-4495
                Publication date Created: May 19 2004
                Publication date (Print): May 19 2004
                Volume: 32
                Issue: 1
                Pages: 111-149
                Article
                DOI: 10.1146/annurev.earth.32.082503.144359
                SO-VID: 859f06ef-e26f-40a8-9b50-00e358882d56
                Copyright © © 2004
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