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  • 1
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    Mantle viscosity (1989)
    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)
    Details
    Publication Date: 1989
    Keywords: earth mantle ; Dynamic ; ConvolutionE ; Plate tectonics ; Inelastic ; Rheology
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    BIBLIOGRAPHY SEISMOLOGY
  • 2
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    Constraints on mantle viscosity from relative sea level variations in Hudson Bay (1992)
    In:  Geophys. Res. Lett., Luxembourg, Conseil de l'Europe, vol. 142, no. 1, pp. 1185-1188, pp. L09610, (ISSN: 1340-4202)
    Details
    Publication Date: 1992
    Keywords: Rheology ; post-glacial ; uplift ; load ; Inelastic ; Modelling
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    BIBLIOGRAPHY SEISMOLOGY
  • 3
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    Constraints on mantle viscosity based upon the inversion of post-glacial uplift data from the Hudson Bay region (1995)
    In:  Geophys. J. Int., Luxembourg, Conseil de l'Europe, vol. 122, no. 1, pp. 353-377, pp. L09610, (ISSN: 1340-4202)
    Details
    Publication Date: 1995
    Keywords: Rheology ; Inelastic ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; GJI
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    BIBLIOGRAPHY SEISMOLOGY
  • 4
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    Constraint on deep mantle viscosity from Lageos acceleration data (1983)
    In:  Nature, Basle, Wiley, vol. 304, no. 6, pp. 434-436, pp. L06315, (ISSN: 1340-4202)
    Details
    Publication Date: 1983
    Keywords: Rheology ; Inelastic ; Gravimetry, Gravitation ; Crustal deformation (cf. Earthquake precursor: deformation or strain)
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    BIBLIOGRAPHY SEISMOLOGY
  • 5
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    Mantle rheology, constitution, and convection (1989)
    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.)
    Details
    Publication Date: 1989
    Keywords: earth mantle ; Dynamic ; ConvolutionE ; Inelastic ; Rheology ; Earth model, also for more shallow analyses !
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    BIBLIOGRAPHY SEISMOLOGY
  • 6
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    Inferences of mantle viscosity from tectonic plate velocities (1991)
    In:  Geophys. Res. Lett., Tokyo, Terra Scientific Publishing Company, vol. 18, no. 17, pp. 1747-1750, pp. 8010, (ISBN: 0534351875, 2nd edition)
    Details
    Publication Date: 1991
    Keywords: Elasticity ; Inelastic ; Plate tectonics ; GRL ; Dziewonski
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    BIBLIOGRAPHY SEISMOLOGY
  • 7
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    Postglacial variations in the level of the sea: Implications for climate dynamics and solid-earth geophysics (1998)
    In:  Rev. Geophys., Basle, Wiley, vol. 36, no. 4, pp. 603-689, pp. L06315, (ISSN: 1340-4202)
    Details
    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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    BIBLIOGRAPHY SEISMOLOGY
  • 8
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    The impulse response of a Maxwell earth (1974)
    In:  Rev. Geophys. Space Phys., Basle, Wiley, vol. 12, no. 6, pp. 649-669, pp. L06315, (ISSN: 1340-4202)
    Details
    Publication Date: 1974
    Keywords: Rheology ; Inelastic ; Review article
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    BIBLIOGRAPHY SEISMOLOGY
  • 9
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    Glacial isostatic adjustment, relative sea level history and mantle viscosity: reconciling relative sea level model predictions for the U.S. East coast with geological constraints (2015)
    Oxford University Press
    Details
    Publication Date: 2015-03-27
    Description: Models of the glacial isostatic adjustment process, which is dominated by the influence of the Late Pleistocene cycle of glaciation and deglaciation, depend on two fundamental inputs: a history of ice-sheet loading and a model of the radial variation of mantle viscosity. These models may be tested and refined by comparing their local predictions of relative sea level history to geological inferences based upon appropriate sea level indicators. The U.S. Atlantic coast is a region of particular interest in this regard, due to the fact that data from the length of this coast provides a transect of the forebulge associated with the former Laurentide ice sheet. High-quality relative sea level histories from this region are employed herein to explore the ability of current models of mantle viscosity to explain the inferred evolution of relative sea level that have accompanied forebulge collapse following deglaciation. Existing misfits are characterized, and alternatives are explored for their reconciliation. It is demonstrated that a new model of mantle viscosity, referred to herein as VM6, when coupled with the latest model of deglaciation history ICE-6G_C, is able to eliminate the majority of these misfits, while continuing to reconcile a wide range of other important geophysical observables, as well as additional relative sea level data from the North American. West coast which also record the collapse of the forebulge but which have not been employed in tuning the viscosity profile to enable ICE-6G_C (VM6) to fit the East coast data set.
    Keywords: Geodynamics and Tectonics
    Print ISSN: 0956-540X
    Electronic ISSN: 1365-246X
    Topics: Geosciences
    Published by Oxford University Press on behalf of The Deutsche Geophysikalische Gesellschaft (DGG) and the Royal Astronomical Society (RAS).
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    PAPER CURRENT
  • 10
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    Glacial isostatic adjustment, relative sea level history and mantle viscosity: reconciling relative sea level model predictions for the U.S. East coast with geological constraints (2015)
    Oxford University Press
    Details
    Publication Date: 2015-03-29
    Description: Models of the glacial isostatic adjustment process, which is dominated by the influence of the Late Pleistocene cycle of glaciation and deglaciation, depend on two fundamental inputs: a history of ice-sheet loading and a model of the radial variation of mantle viscosity. These models may be tested and refined by comparing their local predictions of relative sea level history to geological inferences based upon appropriate sea level indicators. The U.S. Atlantic coast is a region of particular interest in this regard, due to the fact that data from the length of this coast provides a transect of the forebulge associated with the former Laurentide ice sheet. High-quality relative sea level histories from this region are employed herein to explore the ability of current models of mantle viscosity to explain the inferred evolution of relative sea level that have accompanied forebulge collapse following deglaciation. Existing misfits are characterized, and alternatives are explored for their reconciliation. It is demonstrated that a new model of mantle viscosity, referred to herein as VM6, when coupled with the latest model of deglaciation history ICE-6G_C, is able to eliminate the majority of these misfits, while continuing to reconcile a wide range of other important geophysical observables, as well as additional relative sea level data from the North American. West coast which also record the collapse of the forebulge but which have not been employed in tuning the viscosity profile to enable ICE-6G_C (VM6) to fit the East coast data set.
    Keywords: Geodynamics and Tectonics
    Print ISSN: 0956-540X
    Electronic ISSN: 1365-246X
    Topics: Geosciences
    Published by Oxford University Press on behalf of The Deutsche Geophysikalische Gesellschaft (DGG) and the Royal Astronomical Society (RAS).
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