Seismic tomography, surface uplift, and the breakup of Gondwanaland: Integrating mantle convection backwards in time

Author:

Conrad Clinton P.1,Gurnis Michael2

Affiliation:

1. Seismological Laboratory; California Institute of Technology; Pasadena California USA

2. California Institute of Technology; Seismological Laboratory; 1200 E. California Blvd., MC 252-21, Pasadena California 91125 USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference60 articles.

1. Gross thermodynamics of heat engines in deep interior of Earth;Backus;Proc. Natl. Acad. Sci. U.S.A.,1975

2. Thermal constraints on the survival of primitive blobs in the lower mantle;Becker;Earth Planet. Sci. Lett.,1999

3. Tomographic evidence for a narrow whole mantle plume below Iceland;Bijwaard;Earth Planet. Sci. Lett.,1999

4. The backward problem of plate tectonics and mantle convection;Bunge;Eos Trans. AGU,1992

5. Time scales and heterogeneous structure in geodynamic Earth models;Bunge;Science,1998

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