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    Schweizerbart Science Publishers
    In:  Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen, 236 (1-2). pp. 173-183.
    Publication Date: 2017-02-20
    Description: On the central Chilean continental margin off Valparaiso a temporary marine seismological network on the incoming Nazca Plate was supplemented by the Central Chilean Network and a number of temporary landstations. Simultaneous inversion of the complete marine earthquake data set yielded hypocenter distributions from minimum 1-D modeling. These show a considerable seismic activity within the 15 km - 60 km depth range with a maximum number of events between 20 km and 40 km. The distribution shows three areas of increased activity: the O'Higgins Seamount Group on the oceanic plate, the San Antonio Canyon and the northeastern portion of the Valparaiso Basin. There is a marked difference in the distance between the trench and the onset of seismic activity between the San Antonio Canyon area and the Valparaiso Basin area.
    Type: Article , PeerReviewed
    Format: text
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