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    UID:
    gbv_1010124374
    Format: XXV, 213 Seiten , Diagramme, Illustrationen
    Content: Rapidly uplifting coastlines are frequently associated with convergent tectonic boundaries, like subduction zones, which are repeatedly breached by giant megathrust earthquakes. The coastal relief along tectonically active realms is shaped by the effect of sea-level variations and heterogeneous patterns of permanent tectonic deformation, which are accumulated through several cycles of megathrust earthquakes. However, the correlation between earthquake deformation patterns and the sustained long-term segmentation of forearcs, particularly in Chile, remains poorly understood. Furthermore, the methods used to estimate permanent deformation from geomorphic markers, like marine terraces, have remained qualitative and are based on unrepeatable methods. This contrasts with the increasing resolution of digital elevation models, such as Light Detection and Ranging (LiDAR) and high-resolution bathymetric surveys. Throughout this thesis I study permanent deformation in a holistic manner: from the methods to assess deformation rates ...
    Note: Dissertation Universität Potsdam 2016
    Additional Edition: Erscheint auch als Online-Ausgabe Jara Muñoz, Julius, 1979 - Quantifying forearc deformation patterns using coastal geomorphic markers Potsdam, 2016
    Language: English
    Keywords: Zentralchile ; Hebung ; Erdbebenzone ; Küstengebiet ; Störung ; Terrasse ; Provinz Maule ; Hebungsgebiet ; Strandterrasse ; MATLAB ; Modellierung ; Hochschulschrift
    Author information: Strecker, Manfred 1955-
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