Paleomagnetic Evidence for Upper Plate Response To a Step Fault, Sw Anatolia

dc.contributor.author Kaymakci, Nuretdin
dc.contributor.author Langereis, Cor
dc.contributor.author Ozkaptan, Murat
dc.contributor.author Ozacar, A. Arda
dc.contributor.author Gulyuz, Erhan
dc.contributor.author Uzel, Bora
dc.contributor.author Sozbilir, Hasan
dc.date.accessioned 2025-05-10T17:04:11Z
dc.date.available 2025-05-10T17:04:11Z
dc.date.issued 2018
dc.description Ozacar, A. Arda/0000-0001-9700-4400; Gulyuz, Erhan/0000-0002-1539-7982; Uzel, Bora/0000-0003-1703-5026; Kaymakci, Nuretdin/0000-0002-7618-0226 en_US
dc.description.abstract Pliny-Strabo Trench is a Subduction Transform-Edge Propagator (STEP) Fault developed on the northern edge of the subducted African Oceanic Lithosphere. It connects the Aegean and Cyprian trenches in the Eastern Mediterranean convergent system. Although, deep geometry of the STEP fault and associated slab tear in mantle are imaged, its shallow vertical and lateral continuation in the crust and impact on the over-riding plate are still unknown. Thus, we have studied SW Anatolia, the candidate site where this structure could propagate laterally and vertically, for its vertical axis rotations using paleomagnetic tools. In this study, more than 2000 paleomagnetic samples were collected and analysed from 86 different sites which were later classified into 11 separate geographic domains displaying similar tectonic characteristics. Moreover, available paleomagnetic data in the literature were parametrically resampled, analysed and combined with our data. In the region, there is a positive correlation between rotation amounts and sample ages supporting continuous deformation throughout the Neogene period. The spatial variations of results indicated that the study area can be divided into three main domains based on vertical axis rotations. From the south to the north these domains include SW Anatolian domain with similar to 20 degrees counter-clockwise rotation, Burdur-Dinar-Ulubey domain with similar to 4 degrees counter-clockwise rotation and northern areas characterized by clockwise rotations. The identified domains of counter-clockwise rotation are separated by a well-defined NW-SE striking Acipayam Transfer Zone and there is no differential rotation in agreement with the presence of NE-SW striking shear zone in the region. Therefore, we concluded that the Pliny-Strabo STEP Fault have not propagated into the over-riding plate as a shear zone. This implies that there is no evidence to support the presence of alleged Fethiye-Burdur Fault Zone as suggested, and its existence is dubious. (C) 2018 Elsevier B.V. All rights reserved. en_US
dc.description.sponsorship Scientific and Technological Research Council of Turkey [TUBITAK - 111Y239] en_US
dc.description.sponsorship This study is supported by Scientific and Technological Research Council of Turkey, Grant number TUBITAK - 111Y239. We would like to thank Pinar Ertepinar and Ayten Koc for field assistance. en_US
dc.identifier.doi 10.1016/j.epsl.2018.06.022
dc.identifier.issn 0012-821X
dc.identifier.issn 1385-013X
dc.identifier.scopus 2-s2.0-85049495704
dc.identifier.uri https://doi.org/10.1016/j.epsl.2018.06.022
dc.identifier.uri https://hdl.handle.net/20.500.14720/5925
dc.language.iso en en_US
dc.publisher Elsevier Science Bv en_US
dc.rights info:eu-repo/semantics/openAccess en_US
dc.subject Step Fault en_US
dc.subject Pliny-Strabo Trench en_US
dc.subject Sw Anatolia en_US
dc.subject Fethiye Burdur Fault Zone en_US
dc.subject Paleomagnetism en_US
dc.subject Vertical Axis Rotation en_US
dc.title Paleomagnetic Evidence for Upper Plate Response To a Step Fault, Sw Anatolia en_US
dc.type Article en_US
dspace.entity.type Publication
gdc.author.id Ozacar, A. Arda/0000-0001-9700-4400
gdc.author.id Gulyuz, Erhan/0000-0002-1539-7982
gdc.author.id Uzel, Bora/0000-0003-1703-5026
gdc.author.id Kaymakci, Nuretdin/0000-0002-7618-0226
gdc.author.scopusid 6602784664
gdc.author.scopusid 7004123729
gdc.author.scopusid 56499328800
gdc.author.scopusid 55941618800
gdc.author.scopusid 55324918700
gdc.author.scopusid 25222242400
gdc.author.scopusid 25222242400
gdc.author.wosid Sozbilir, Hasan/Aah-1741-2019
gdc.author.wosid Uzel, Bora/J-7317-2016
gdc.author.wosid Özkaptan, Murat/Aae-8071-2019
gdc.author.wosid Ozacar, A. Arda/Aaz-8730-2020
gdc.author.wosid Kaymakci, Nuretdin/B-3830-2014
gdc.coar.access open access
gdc.coar.type text::journal::journal article
gdc.description.department T.C. Van Yüzüncü Yıl Üniversitesi en_US
gdc.description.departmenttemp [Kaymakci, Nuretdin; Ozacar, A. Arda] Middle East Tech Univ METU ODTU, Dept Geol Engn, Dumlupinar Bulvari 1, TR-06800 Ankara, Turkey; [Langereis, Cor] Univ Utrecht, Dept Earth Sci, Budapestlaan 17, NL-3584 CD Utrecht, Netherlands; [Ozkaptan, Murat] Karadeniz Tech Univ, Dept Geophys Engn, TR-61080 Trabzon, Turkey; [Gulyuz, Erhan] Van Yuzuncuyil Univ, Dept Geol Engn, TR-65080 Van, Turkey; [Uzel, Bora; Sozbilir, Hasan] Dokuz Eylul Univ, Dept Geol Engn, Tinaztepe Campus, TR-35160 Izmir, Turkey en_US
gdc.description.endpage 115 en_US
gdc.description.publicationcategory Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı en_US
gdc.description.scopusquality Q1
gdc.description.startpage 101 en_US
gdc.description.volume 498 en_US
gdc.description.woscitationindex Science Citation Index Expanded
gdc.description.wosquality Q1
gdc.identifier.wos WOS:000442060600010
gdc.index.type WoS
gdc.index.type Scopus

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