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A new mechanical model for Tibet

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  • Jeffrey T. Freymueller

    (Jeffrey T. Freymueller is at the Geophysical Institute, University of Alaska Fairbanks, Fairbanks, Alaska 99775, USA.)

Abstract

A three-dimensional mechanical model of the Tibetan crust explains both the first-order features of GPS surface velocities and the contrast in the types of earthquake between northern and southern Tibet. See Letter p.79

Suggested Citation

  • Jeffrey T. Freymueller, 2011. "A new mechanical model for Tibet," Nature, Nature, vol. 472(7341), pages 48-49, April.
    • Handle: RePEc:nat:nature:v:472:y:2011:i:7341:d:10.1038_472048a
    DOI: 10.1038/472048a
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