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Abstrakty
A detailed investigation of microseismicity and fault plane solutions are used to determine the current tectonic activity of the prominent zone of seismicity near Samos Island and Kusadasi Bay. The activation of fault populations in this complex strike-slip and normal faulting system was investigated by using several thousand accurate earthquake locations obtained by applying a double-difference location method and waveform cross-correlation, appropriate for areas with relatively small seismogenic structures. The fault plane solutions, determined by both moment tensor waveform inversions and P-wave first motion polarities, reveal a clear NS trending extension direction, for strike slip, oblique normal and normal faults. The geometry of each segment is quite simple and indicates planar dislocations gently dipping with an average dip of 40-45°, maintaining a constant dip through the entire seismogenic layer, down to 15 km depth.
Wydawca
Czasopismo
Rocznik
Tom
Strony
1283--1309
Opis fizyczny
Bibliogr. 29 poz.
Twórcy
autor
- TÜBİTAK Marmara Research Center, Earth and Marine Sciences Institute, Gebze, Turkey
autor
- Geophysics Department, School of Geology, Aristotle University of Thessaloniki, Thessaloniki
autor
- TÜBİTAK Marmara Research Center, Earth and Marine Sciences Institute, Gebze, Turkey
autor
- Geophysics Department, School of Geology, Aristotle University of Thessaloniki, Thessaloniki
autor
- TÜBİTAK Marmara Research Center, Earth and Marine Sciences Institute, Gebze, Turkey
autor
- Geophysics Department, School of Geology, Aristotle University of Thessaloniki, Thessaloniki
Bibliografia
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-0b58c7c3-e804-4583-8a91-fee121d6ddb3