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  • 1
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    Gordon and Breach
    In:  Bull., Open-File Rept., Mantle Convection: Plate Tectonics and Global Dynamics, New York, Gordon and Breach, vol. 4, no. 1, pp. 389-478, (ISBN 0080419208)
    Publication Date: 1989
    Keywords: earth mantle ; Dynamic ; ConvolutionE ; Plate tectonics ; Inelastic ; Rheology
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  • 2
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    In:  Geophys. Res. Lett., Luxembourg, Conseil de l'Europe, vol. 142, no. 1, pp. 1185-1188, pp. L09610, (ISSN: 1340-4202)
    Publication Date: 1992
    Keywords: Rheology ; post-glacial ; uplift ; load ; Inelastic ; Modelling
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  • 3
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    In:  Geophys. J. Int., Luxembourg, Conseil de l'Europe, vol. 122, no. 1, pp. 353-377, pp. L09610, (ISSN: 1340-4202)
    Publication Date: 1995
    Keywords: Rheology ; Inelastic ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; GJI
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  • 4
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    In:  Nature, Basle, Wiley, vol. 304, no. 6, pp. 434-436, pp. L06315, (ISSN: 1340-4202)
    Publication Date: 1983
    Keywords: Rheology ; Inelastic ; Gravimetry, Gravitation ; Crustal deformation (cf. Earthquake precursor: deformation or strain)
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  • 5
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    Gordon and Breach
    In:  Professional Paper, Mantle Convection: Plate Tectonics and Global Dynamics, New York, Gordon and Breach, vol. 4, no. 16, pp. 595-655, (ISBN 1-86239-165-3, vi + 330 pp.)
    Publication Date: 1989
    Keywords: earth mantle ; Dynamic ; ConvolutionE ; Inelastic ; Rheology ; Earth model, also for more shallow analyses !
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  • 6
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    In:  Geophys. Res. Lett., Tokyo, Terra Scientific Publishing Company, vol. 18, no. 17, pp. 1747-1750, pp. 8010, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1991
    Keywords: Elasticity ; Inelastic ; Plate tectonics ; GRL ; Dziewonski
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  • 7
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    In:  Rev. Geophys., Basle, Wiley, vol. 36, no. 4, pp. 603-689, pp. L06315, (ISSN: 1340-4202)
    Publication Date: 1998
    Keywords: Inelastic ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Rheology ; earth mantle ; isostasy ; Earth rotation ; Geodesy ; 1236 ; Geodesy ; and ; gravity ; Rheology ; of ; the ; lithosphere ; and ; mantle ; (8160) ; 4556 ; Oceanography: ; Physical ; Sea ; level ; variations ; 3260 ; Mathematical ; geophysics ; Inverse ; theory
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  • 8
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    In:  Rev. Geophys. Space Phys., Basle, Wiley, vol. 12, no. 6, pp. 649-669, pp. L06315, (ISSN: 1340-4202)
    Publication Date: 1974
    Keywords: Rheology ; Inelastic ; Review article
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  • 9
    Publication Date: 2016-06-07
    Description: Recent interpretations of laser ranging for the LAGEOS satellite have rather conclusively established that the observed acceleration in the node of its orbit is just that expected to exist as a residual effect of the last deglaciation event which ended about 6000 years ago. The nontidal acceleration of rotation would be rather different than that observed if there were any significant melting of high latitude continental ice masses currently ongoing. The sensitivity of the expected nontidal acceleration to variations of several elements of the radial viscoelastic structure of the planet is explored using a new normal mode method for the computation of viscoelastic relaxation spectra. These calculations establish that the most important sensitivity is to variations in the mantle viscosity profile. Although the predicted nontidal acceleration does depend upon lithospheric thickness and on the elastic component of the radial structure, the dependence on these components of the structure is much weaker than it is upon mantle viscosity. The observed J sub 2 is therefore a particularly useful determinant of radial variations in the latter parameter.
    Keywords: GEOPHYSICS
    Type: NASA, Washington Geopotential Res. Mission (GRM); p 71
    Format: application/pdf
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  • 10
    Publication Date: 2016-06-07
    Description: The connection between the observed large scale structure of the Earths' gravitational field, as represented by the GEM10 model, and the surface kinematic manifestations of plate tectonics, as represented by the absolute plate motion model of Minster and Jordan, is explored using a somewhat novel method of analysis. Two scalar derivatives of the field of surface plate velocities, namely the horizontal divergence and the radial vorticity, are computed from the plate motion data. These two scalars are respectively determined by the poloidal and toroidal scalars in terms of which any essentially solenoidal vector field may be completely represented. They provide a compact summary of the observed plate boundary types in nature, with oceanic ridges and trenches being essentially boundaries of divergence, and transform faults being essentially boundaries of vorticity.
    Keywords: GEOPHYSICS
    Type: NASA, Washington Geopotential Res. Mission (GRM); p 63
    Format: application/pdf
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