Microearthquake hypocenter determination in the southern Aegean Sea from records of sea-floor and land-based seismographs

Details Microearthquake hypocenter determination in the southern Aegean Sea from records of sea-floor and land-based seismographs Microearthquake hypocenter determination in the southern Aegean Sea from records of sea-floor and land-based seismographs

Dec 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992pepi...75..177s&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 75, Issue 1-3, p. 177-183.

Physics

1

Scientific paper

During the cruise of the Soviet research vessel RIFT in April 1987 in the southern Aegean Sea, an array of five ocean bottom seismographs was deployed. During its operation (19-27 April), more than 400 events with magnitudes, ML, varying between -0.5 and 4.4 were recorded. Their spatial distribution reconfirms the typical characteristics of a subducting slab (Mediterranean lithosphere) under the Aegean lithosphere. The thickness of the seismogenic layer in the southern Aegean sea is of the order of 30 km.

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