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  • Book  (2)
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  • 1
    UID:
    gbv_1676217703
    Format: 192 Seiten , Illustrationen, Diagramme
    Content: Continental rift systems open up unique possibilities to study the geodynamic system of our planet: geodynamic localization processes are imprinted in the morphology of the rift by governing the time-dependent activity of faults, the topographic evolution of the rift or by controlling whether a rift is symmetric or asymmetric. Since lithospheric necking localizes strain towards the rift centre, deformation structures of previous rift phases are often well preserved and passive margins, the end product of continental rifting, retain key information about the tectonic history from rift inception to continental rupture. Current understanding of continental rift evolution is based on combining observations from active rifts with data collected at rifted margins. Connecting these isolated data sets is often accomplished in a conceptual way and leaves room for subjective interpretation. Geodynamic forward models, however, have the potential to link individual data sets in a quantitative manner, using additional constraints from rock mechanics and rheology, which allows to transcend previous conceptual models of rift evolution. ...
    Note: Enthält 20 Publikationen , Habilitationsschrift Universität Potsdam 2019
    Additional Edition: Erscheint auch als Online-Ausgabe Brune, Sascha, 1980 - Modelling continental rift dynamics Potsdam, 2018
    Language: English
    Keywords: Kontinentale Erdkruste ; Rifting ; Riftsystem ; Geodynamik ; Modellierung ; Plattentektonik ; Geodynamik ; Rift ; Hochschulschrift
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  • 2
    UID:
    gbv_1733457518
    Format: vii, 120 Seiten , Illustrationen, Diagramme, Karten
    Content: After a severe M W 5.7 earthquake on October 17, 2015 in El Galpón in the province of Salta NW Argentina, I installed a local seismological network around the estimated epicenter. The network covered an area characterized by inherited Cretaceous normal faults and neotectonic faults with unknown recurrence intervals, some of which may have been reactivated normal faults. The 13 three-component seismic stations recorded data continuously for 15 months. The 2015 earthquake took place in the Santa Bárbara System of the Andean foreland, at about 17km depth. This region is the easternmost morphostructural region of the central Andes. As a part of the broken foreland, it is bounded to the north by the Subandes fold-and-thrust belt and the Sierras Pampeanas to the south; to the east lies the Chaco-Paraná basin. A multi-stage morphotectonic evolution with thick-skinned basement uplift and coeval thin-skinned deformation in the intermontane basins is suggested for the study area. The release of stresses associated with the foreland ...
    Note: Dissertation Universität Potsdam 2020
    Additional Edition: Erscheint auch als Online-Ausgabe Zeckra, Martin Seismological and seismotectonic analysis of the northwestern Argentine Central Andean foreland Potsdam, 2020
    Language: English
    Keywords: Provinz Salta ; Erdbeben ; Vorland ; Seismotektonik ; Störung ; Neotektonik ; Argentinien ; Zentralanden ; Seismologie ; Erdbebenzone ; Seismometrie ; Orientierung ; Tektonik ; Provinz Salta ; Datenauswertung ; Deformation ; Erdbebenherd ; Hochschulschrift
    Library Location Call Number Volume/Issue/Year Availability
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