Browsing by Subject "Passive und aktive Kontinentalränder {Geologie}"
Now showing items 1-17 of 17
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Charakterisierung eines vulkanisch geprägten passiven Kontinentalrandes mit seismischen Verfahren am Beispiel Namibias
(GFZ, Helmholtz-Zentrum, 2001)
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Crustal structure modelling and interpretation of the East Greenland continental margin between 72°N and 77°N
(Univ. Bremen, 2008)Integrated studies of conjugate margins provide important constraints for the sequence of events of synrift tectonic and magmatic processes. The northeast Greenland margin is investigated based on seismic refraction data ... -
Deformationsanalyse und mechanische Kopplung eines aktiven fore-arcs in Raum und Zeit, Kamtschatka, Russische Föderation
(11. Symposium "Tektonik, Struktur- und Kristallingeologie", 2006-03)Seit dem Mesozoikum wächst die kontinentale Kruste am aktiven Plattenrand von Kamtschatka durch Akkretion allochthoner Terrane. Dieses Wachstum manifestiert sich in der differenziellen Exhumierung und Hebung tektonischer Blöcke ... -
Gravity and magnetic investigations along the Peruvian continental margin
(Univ. Hamburg, 2002)This work presents the first three-dimensional gravity and magnetic investigation along the convergent Peruvian margin. Three-dimensional magnetic modelling is still a relatively untried and challenging technique. The ... -
Integrating structural and sedimentological observations with numerical lithospheric models to assess the 3D evolution of the South African continental passive margin
(GFZ, Helmholtz-Zentrum, Potsdam, 2008) -
Inversion of gravity data with application to density modeling of the Hellenic subduction zone
(Univ. Bochum, 2005)Diese Arbeit beschäftigt sich mit der Verknüpfung von manuellen und automatischen Inversionmethoden für die Interpretation gravimetrischer Anomalien. Eine neue Software mit dem Namen 3GRAINS wird vorgestellt. Sie wurde für ... -
Kinematik und Dynamik neogener Deformationsprozesse des südzentralchilenischen Subduktionssystems, nördlichste Patagonische Anden (37° - 40° S)
(Univ. Hamburg, 2003)Die dynamische Entwicklung des neotektonisch und vulkanisch aktiven südchilenischen Plattenrandes wird durch die schiefe Subduktion der ozeanischen Nazca Platte unter den südamerikanischen Kontinent gesteuert. Die Deformationen ... -
Lithospheric structure of the Aegean obtained from P and S receiver functions
(Scientific Technical Report / Geoforschungszentrum Potsdam; 2005, 15) -
Marine gravimetric and magnetic investigations within the area of the southeastern Mediterranean Sea and the northern section of Egypt
(Univ. Hamburg, 2004)The southeastern Mediterranean Sea and the northern section of Egypt constitutes one of the most complex tectonic areas in the Mediterranean. This study is an attempt to achieve a better understanding of tectonics, and ... -
Near-surface sediment structures at cold seeps and their physical control on seepage - a geophysical and geological study in the southern Gulf of Mexico and at the frontal Makran Accretionary prism, Pakistan
(Univ. Bremen, 2009)The major objective of the study is to investigate how near-surface sediment structures and other geological aspects control the nature and occurrence of cold fluid seepage. Mainly high resolution multichannel seismic data ... -
Scale related strain evolution at convergent margins and effects due to parameter changes - insights from nature and experiment
(GFZ, Helmholtz-Zentrum[Bibliothek des Wiss.-Parks Albert Einstein] [Vertrieb], [Potsdam], 2007) -
Seismic structure of the Central Andean subduction zone from local earthquake data
(GFZ, Helmholtz-Zentrum, 2001)
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Tectonic and magmatic processes along the transform margin of Southern Africa
(Univ. Bremen, 2009)Giant shear processes shaped Africa's southern margin during the breakup of the supercontinent Gondwana. They acted along a more than 1000 km long transform fault, whose remnant structure the Agulhas-Falkland Fracture ...
