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  • Inelastic  (8)
  • Geodynamics and Tectonics  (3)
  • 1
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    Unbekannt
    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)
    Publikationsdatum: 1989
    Schlagwort(e): earth mantle ; Dynamic ; ConvolutionE ; Plate tectonics ; Inelastic ; Rheology
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
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    Unbekannt
    In:  Geophys. Res. Lett., Luxembourg, Conseil de l'Europe, vol. 142, no. 1, pp. 1185-1188, pp. L09610, (ISSN: 1340-4202)
    Publikationsdatum: 1992
    Schlagwort(e): Rheology ; post-glacial ; uplift ; load ; Inelastic ; Modelling
    Standort Signatur Erwartet Verfügbarkeit
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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)
    Publikationsdatum: 1995
    Schlagwort(e): Rheology ; Inelastic ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; GJI
    Standort Signatur Erwartet Verfügbarkeit
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  • 4
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    Unbekannt
    In:  Nature, Basle, Wiley, vol. 304, no. 6, pp. 434-436, pp. L06315, (ISSN: 1340-4202)
    Publikationsdatum: 1983
    Schlagwort(e): Rheology ; Inelastic ; Gravimetry, Gravitation ; Crustal deformation (cf. Earthquake precursor: deformation or strain)
    Standort Signatur Erwartet Verfügbarkeit
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  • 5
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    Unbekannt
    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.)
    Publikationsdatum: 1989
    Schlagwort(e): earth mantle ; Dynamic ; ConvolutionE ; Inelastic ; Rheology ; Earth model, also for more shallow analyses !
    Standort Signatur Erwartet Verfügbarkeit
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  • 6
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    Unbekannt
    In:  Geophys. Res. Lett., Tokyo, Terra Scientific Publishing Company, vol. 18, no. 17, pp. 1747-1750, pp. 8010, (ISBN: 0534351875, 2nd edition)
    Publikationsdatum: 1991
    Schlagwort(e): Elasticity ; Inelastic ; Plate tectonics ; GRL ; Dziewonski
    Standort Signatur Erwartet Verfügbarkeit
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  • 7
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    Unbekannt
    In:  Rev. Geophys., Basle, Wiley, vol. 36, no. 4, pp. 603-689, pp. L06315, (ISSN: 1340-4202)
    Publikationsdatum: 1998
    Schlagwort(e): 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
    Standort Signatur Erwartet Verfügbarkeit
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  • 8
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    Unbekannt
    In:  Rev. Geophys. Space Phys., Basle, Wiley, vol. 12, no. 6, pp. 649-669, pp. L06315, (ISSN: 1340-4202)
    Publikationsdatum: 1974
    Schlagwort(e): Rheology ; Inelastic ; Review article
    Standort Signatur Erwartet Verfügbarkeit
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  • 9
    Publikationsdatum: 2015-03-27
    Beschreibung: 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.
    Schlagwort(e): Geodynamics and Tectonics
    Print ISSN: 0956-540X
    Digitale ISSN: 1365-246X
    Thema: Geologie und Paläontologie
    Publiziert von Oxford University Press im Namen von The Deutsche Geophysikalische Gesellschaft (DGG) and the Royal Astronomical Society (RAS).
    Standort Signatur Erwartet Verfügbarkeit
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  • 10
    Publikationsdatum: 2015-03-29
    Beschreibung: 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.
    Schlagwort(e): Geodynamics and Tectonics
    Print ISSN: 0956-540X
    Digitale ISSN: 1365-246X
    Thema: Geologie und Paläontologie
    Publiziert von Oxford University Press im Namen von The Deutsche Geophysikalische Gesellschaft (DGG) and the Royal Astronomical Society (RAS).
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
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