Kinematics of the East Anatolian Fault Zone between Turkoglu (Kahramanmaras) and Celikhan (Adiyaman), eastern Turkey
dc.contributor.author | Yilmaz, Huseyin | |
dc.contributor.author | Over, Semir | |
dc.contributor.author | Ozden, Suha | |
dc.date.accessioned | 2024-09-18T19:54:18Z | |
dc.date.available | 2024-09-18T19:54:18Z | |
dc.date.issued | 2006 | |
dc.department | Hatay Mustafa Kemal Üniversitesi | en_US |
dc.description.abstract | In this study we determined the stress regime acting along the East Anatolian Fault Zone between Turkoglu (Kahramanmaras) and Celikhan (Adiyaman), from the Neocene to present-day, based on the inversion of striations measured on faults and on the focal mechanisms of earthquakes having magnitudes greater than 5.0. The inversions yield a strike-slip stress regime with a reverse component (i.e., transpression) operative in the Neocene to present with a consistent N-to NW-trending or, axis 156 +/- 11 degrees and an E- to NE-trending sigma(3) axis, sigma(7) 9 degrees sigma(3), producing left-lateral motion along the East Anatolian Fault Zone. The inversions of focal mechanisms yield a strike-slip stress deviator characterized by an approximately N-S (N1 degrees W)-trending sigma(1), and an approximately E-W (N89 degrees E)-trending sigma(3) axis. Both the kinematic analysis and structural observations indicate that the stress regime operating in the study area has had a transpressional character, giving rise to the Mio-Pliocene compressive structures (reverse faults, thrusts and folds) observed in the study area. Field observations allow estimation of a Pliocene age for the strike-slip East Anatolian Fault Zone. | en_US |
dc.identifier.doi | 10.1186/BF03352645 | |
dc.identifier.endpage | 1473 | en_US |
dc.identifier.issn | 1880-5981 | |
dc.identifier.issue | 11 | en_US |
dc.identifier.scopus | 2-s2.0-33846940761 | en_US |
dc.identifier.scopusquality | Q1 | en_US |
dc.identifier.startpage | 1463 | en_US |
dc.identifier.uri | https://doi.org/10.1186/BF03352645 | |
dc.identifier.uri | https://hdl.handle.net/20.500.12483/7647 | |
dc.identifier.volume | 58 | en_US |
dc.identifier.wos | WOS:000243442500004 | en_US |
dc.identifier.wosquality | Q3 | en_US |
dc.indekslendigikaynak | Web of Science | en_US |
dc.indekslendigikaynak | Scopus | en_US |
dc.language.iso | en | en_US |
dc.publisher | Springer | en_US |
dc.relation.ispartof | Earth Planets and Space | en_US |
dc.relation.publicationcategory | Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı | en_US |
dc.rights | info:eu-repo/semantics/openAccess | en_US |
dc.subject | Anatolia | en_US |
dc.subject | East Anatolian Fault | en_US |
dc.subject | stress state | en_US |
dc.subject | earthquake | en_US |
dc.subject | fault-slip inversion | en_US |
dc.title | Kinematics of the East Anatolian Fault Zone between Turkoglu (Kahramanmaras) and Celikhan (Adiyaman), eastern Turkey | en_US |
dc.type | Article | en_US |
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