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Showing 1 to 7 of 7 for “"Geodynamic model"”.

  1. Geodynamic evolution and petrogenesis of the neoarchaean Francistown granite-greenstone complex in NE Botswana, SW margin of the Zimbabwe craton

    … the NE Botswana, and with which to formulate a geodynamic model for better understanding of the Archaean crustal growth flanking the southwestern margin of the Zimbabwe Craton

    cape-town Repository record for Geodynamic evolution and petrogenesis of the neoarchaean Francistown granite-greenstone complex in NE Botswana, SW margin of the Zimbabwe craton (opens in a new tab)

  2. LATERALLY HETEROGENEOUS SEISMIC ANISOTROPY INVESTIGATED BY SHEAR WAVE SPLITTING ANALYSES

    … at ~ 250 km and can be explained by a simple geodynamic model invoking absolute plate motion related to simple shear in the lithosphere-asthenosphere transitional layer and mantle flow deflected by the thick lithospheric root of the basin in the upper asthenosphere. In the vicinity of the 2019 …

    must-thes Repository record for LATERALLY HETEROGENEOUS SEISMIC ANISOTROPY INVESTIGATED BY SHEAR WAVE SPLITTING ANALYSES (opens in a new tab)

  3. Dynamic links between short-term deformation and long-term tectonics: a finite element study

    … movement. By using 2-D and 3-D finite element models with viscoelastoplastic rheology, I have explored the spatial-temporal strain and stress evolution during seismic cycles, and linked these results to long-term tectonics. In the central Andes, I found that much of the GPS-measured crustal …

    missouri Repository record for Dynamic links between short-term deformation and long-term tectonics: a finite element study (opens in a new tab)

  4. Quantifying slab evolution and mantle flow using global subduction models with data assimilation

    Submission published under a 24 month embargo labeled 'U of I Access', the embargo will last until 2024-05-01

    uiuc Repository record for Quantifying slab evolution and mantle flow using global subduction models with data assimilation (opens in a new tab)

  5. Metamorphic evolution of ultrahigh-temperature granulite facies and upper amphibolite facies rocks of the Epupa Complex, NW Namibia

    … expense of biotite in several paragneisses. In a geodynamic model UHT metamorphism of the Epembe Unit is correlated with the formation of a large magma chamber at the mantle-crust boundary, which forms the source for the anorthosites of the KIC. In contrast, amphibolite facies metamorphism of the …

    wurz-thes Repository record for Metamorphic evolution of ultrahigh-temperature granulite facies and upper amphibolite facies rocks of the Epupa Complex, NW Namibia (opens in a new tab)

  6. Studying subduction zone dynamics and continental evolution in South America using data-oriented geodynamic models

    … restricted to the sampling area. While numerical modeling can largely overcome these shortcomings, it is affected by uncertain model parameters. As a result, many tectonic questions remain open, with little consensus from decades' of dedicated research. One promising way to further investigate the …

    uiuc Repository record for Studying subduction zone dynamics and continental evolution in South America using data-oriented geodynamic models (opens in a new tab)

  7. New Constraints For Convergent Margin Plate Tectonic Reconstructions From Imaged And Predicted Mantle Structure

    Details of global plate models decrease back in geological time, such that approximately one-third of the Earth surface lacks sufficient plate tectonic constraints by the early Cenozoic ~50 Ma, increasing to >60% uncertainty by the Late Jurassic. The most significant global plate model

    houston Repository record for New Constraints For Convergent Margin Plate Tectonic Reconstructions From Imaged And Predicted Mantle Structure (opens in a new tab)