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Deformation patterns in the southwestern part of the Mediterranean Ridge (South Matapan Trench, Western Greece)

Andronikidis Nikolaos, Kokinou, Eleni, Manoutsoglou Emmanouil, Vafeidis Antonios, Καμπέρης Ευάγγελος

Απλή Εγγραφή


URIhttp://purl.tuc.gr/dl/dias/967BE103-1DC5-4151-AFC0-79A4FBF724A6-
Αναγνωριστικόhttps://link.springer.com/article/10.1007%2Fs11001-017-9337-0-
Αναγνωριστικόhttps://doi.org/10.1007/s11001-017-9337-0-
Γλώσσαen-
Μέγεθος17 pagesen
ΤίτλοςDeformation patterns in the southwestern part of the Mediterranean Ridge (South Matapan Trench, Western Greece)en
ΔημιουργόςAndronikidis Nikolaosen
ΔημιουργόςΑνδρονικιδης Νικολαοςel
ΔημιουργόςKokinou, Elenien
ΔημιουργόςManoutsoglou Emmanouilen
ΔημιουργόςΜανουτσογλου Εμμανουηλel
ΔημιουργόςVafeidis Antoniosen
ΔημιουργόςΒαφειδης Αντωνιοςel
ΔημιουργόςΚαμπέρης Ευάγγελοςel
ΔημιουργόςKamberis Evangelosen
ΕκδότηςSpringer Publishing Companyen
ΠερίληψηSeismic reflection data and bathymetry analyses, together with geological information, are combined in the present work to identify seabed structural deformation and crustal structure in the Western Mediterranean Ridge (the backstop and the South Matapan Trench). As a first step, we apply bathymetric data and state of art methods of pattern recognition to automatically detect seabed lineaments, which are possibly related to the presence of tectonic structures (faults). The resulting pattern is tied to seismic reflection data, further assisting in the construction of a stratigraphic and structural model for this part of the Mediterranean Ridge. Structural elements and stratigraphic units in the final model are estimated based on: (a) the detected lineaments on the seabed, (b) the distribution of the interval velocities and the presence of velocity inversions, (c) the continuity and the amplitudes of the seismic reflections, the seismic structure of the units and (d) well and stratigraphic data as well as the main tectonic structures from the nearest onshore areas. Seabed morphology in the study area is probably related with the past and recent tectonics movements that result from African and European plates’ convergence. Backthrusts and reverse faults, flower structures and deep normal faults are among the most important extensional/compressional structures interpreted in the study area.en
ΤύποςPeer-Reviewed Journal Publicationen
ΤύποςΔημοσίευση σε Περιοδικό με Κριτέςel
Άδεια Χρήσηςhttp://creativecommons.org/licenses/by/4.0/en
Ημερομηνία2018-03-05-
Ημερομηνία Δημοσίευσης2017-
Θεματική ΚατηγορίαDeformation patternsen
Θεματική ΚατηγορίαInner Mediterranean Ridgeen
Θεματική ΚατηγορίαSeaflooren
Θεματική ΚατηγορίαSeismic structureen
Θεματική ΚατηγορίαTectonicsen
Βιβλιογραφική ΑναφοράN. Andronikidis, E. Kokinou, A. Vafidis, E. Kamberis and E. Manoutsoglou, "Deformation patterns in the southwestern part of the Mediterranean Ridge (South Matapan Trench, Western Greece)," Mar. Geophys. Res., pp. 1-16, Dec 2017. doi:10.1007/s11001-017-9337-0 en

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