Search Results - "Bribach, J."

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  1. 1

    The refraction seismic experiment GRANU95 in the Saxothuringian belt, southeastern Germany by Enderle, U., Schuster, K., Prodehl, C., Schulze, A., Bribach, J.

    Published in Geophysical journal international (01-05-1998)
    “…In this paper we present newly acquired high‐quality wide‐angle seismic data of the GRANU95 project and first models of the crustal structure along two…”
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    Journal Article
  2. 2

    The crustal structure beneath the Central Andean forearc and magmatic arc as derived from seismic studies — the PISCO 94 experiment in northern Chile (21°–23°S) by Schmitz, M, Lessel, K, Giese, P, Wigger, P, Araneda, M, Bribach, J, Graeber, F, Grunewald, S, Haberland, C, Lüth, S, Röwer, P, Ryberg, T, Schulze, A

    Published in Journal of South American earth sciences (01-11-1999)
    “…In this study, we present an interpretation of seismic refraction profiles from the PISCO 94 experiment in northern Chile. As the PISCO experiment was a…”
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    Journal Article
  3. 3

    The reflection seismic survey of project TIPTEQ—the inventory of the Chilean subduction zone at 38.2° S by Groß, K., Micksch, U.

    Published in Geophysical journal international (01-02-2008)
    “…We describe results of an active-source seismology experiment across the Chilean subduction zone at 38.2°S. The seismic sections clearly show the subducted…”
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    Journal Article
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    Thickness of the lithosphere east of the Dead Sea Transform by Mohsen, Ayman, Kind, Rainer, Sobolev, Stephan V., Weber, Michael

    Published in Geophysical journal international (01-11-2006)
    “…We use the S receiver function method to study the lithosphere at the Dead Sea Transform (DST). A temporary network of 22 seismic broad-band stations was…”
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  6. 6

    Seismic reflection image revealing offset of Andean subduction-zone earthquake locations into oceanic mantle by Group, The ANCORP Working

    Published in Nature (London) (28-01-1999)
    “…Since the advent of plate-tectonic theory over 30 years ago,, the geometries of subduction zones have been constrained mainly by the spatial distribution of…”
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  7. 7