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  • 1
    Electronic Resource
    Electronic Resource
    NIZUSE: a deep seismic reflection line in north-eastern Germany (1994)
    Springer
    International journal of earth sciences 83 (1994), S. 161-169 
    Details
    ISSN: 1437-3262
    Keywords: Deep seismic reflection profiling ; Northeast German Basin ; External Variscides ; North German Massif ; Rugen-Pomorze Terrane
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Out of a dense network of seismic reflection lines for hydrocarbon exploration in the North-east German Basin, several lines were recorded to 12 s TWT to obtain information about the structure of the crust and the crust-mantle transition. One of these profiles is presented here. This stretches for 110 km in a NNE direction between Neustrelitz and the island of Usedom. It reaches from the External Variscides in the south across the North German Massif into the Rügen-Pomorze Terrane in the Baltic Sea. Below Cenozoic-Mesozoic-Paleozoic cover with clear reflections down to base Zechstein, the reflectivity varies considerably with depth and also laterally. The Paleozoic and Precambrian sediments and basement are generally void of reflections, but the lower crust and the Moho show strong reflections. To the north the reflectivity decreases, and the Moho depth increases to beyond the bottom of the record section at 12 s. There are no direct indications for deep-reaching faults such as the Trans-European Fault in the north. The North German Massif acted as a ramp towards the Variscan Orogeny, similar to the London-Brabant Massif further west.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00211899
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    Paper (German National Licenses)
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  • 2
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    Ocean bottom seismics (2011)
    Springer
    In:  In: Encyclopedia of Solid Earth Geophysics, Vol. 1-2. , ed. by Gupta, H. K. Encyclopedia of Earth Sciences Series . Springer, Heidelberg, Germany, pp. 901-918. 1. ed. ISBN 978-90-481-8701-0
    Details
    Publication Date: 2020-08-03
    Type: Book chapter , NonPeerReviewed
    Format: text
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    OceanRep: Book chapter
  • 3
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    Unknown
    The seismogenic zone in the Central Costa Rican Pacific margin: high-quality hypocenters from an amphibious network (2014)
    Springer
    In:  International Journal of Earth Sciences, 103 (7). pp. 1747-1764.
    Details
    Publication Date: 2017-05-23
    Description: Transition from subduction of normal to thickened oceanic crust occurs in the central portion of the Costa Rican margin, where large interplate earthquakes (M * 7) and abundant interseismic seismicity have been associated with subduction of bathymetric highs. We relocated *1,300 earthquakes recorded for 6 months by a combined on- and offshore seismological network using probabilistic earthquake relocation in a 3D P-wave velocity model. Most of the seismicity originated at the seismogenic zone of the plate boundary, appearing as an 18° dipping, planar cluster from 15 to 25–30 km depth, beneath the continental shelf. Several reverse focal mechanisms were resolved within the cluster. The upper limit of this interseismic interplate seismicity seems to be controlled primarily by the overlying-plate thickness and coherency, which in turn is governed by the erosional processes and fluid release and escape at temperatures lower than *100 to 120° C along the plate boundary. The downdip limit of the stick–slip behaviour collocates with relative low temperatures of *150 to 200° C, suggesting that it is controlled by serpentinization of the mantle wedge. The distribution of the interseismic interplate seismicity is locally modified by the presence of subducted seamounts at different depths. Unlike in northern Costa Rica, rupture of large earthquakes in the last two decades seems to coincide with the area defined by the interseismic interplate seismicity.
    Type: Article , PeerReviewed
    Format: text
    DOI: 10.1007/s00531-013-0955-8
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    OceanRep: Article in a Scientific Journal - peer-reviewed
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