1 Ocak 2021 Dergi makalesi Açık Erişim

Tosun, Levent; Avsar, Ulas; Avsar, Ozgur; Dondurur, Derman; Kaymakci, Nuretdin

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  <dc:creator>Tosun, Levent</dc:creator>
  <dc:creator>Avsar, Ulas</dc:creator>
  <dc:creator>Avsar, Ozgur</dc:creator>
  <dc:creator>Dondurur, Derman</dc:creator>
  <dc:creator>Kaymakci, Nuretdin</dc:creator>
  <dc:date>2021-01-01</dc:date>
  <dc:description>Pliny-Strabo Trench (PST)is a Subduction Transform Edge Propagator (STEP) fault developed at the northern edge of the African oceanic lithosphere connecting the Aegean and Cyprian trenches in the eastern Mediterra-nean. Recent studies have demonstrated that the PST terminates close to Turkish Border and links to the Cyprian trench east of Rhodes and south of Fethiye-Gocek Bay. However, it is also claimed that the PST extends into SW Anatolia along a sinistral transtensional shear zone, so-called Fethiye-Burdur Fault Zone (FBFZ) implying that a lithospheric tear in the downgoing plate extends into the over-riding plate, although, this is kinematically almost impossible since full mechanical coupling between down going and the over-riding plate is necessary. To test this hypothesis and understand the kinematics of the transition zone between PST and Cyprian trench we have conducted a rigorous paleostress inversion study combined with interpretation of 2D seismic data of which 228 km total length obtained from Fethiye-Gocek Bay.</dc:description>
  <dc:identifier>https://aperta.ulakbim.gov.trrecord/238284</dc:identifier>
  <dc:identifier>oai:aperta.ulakbim.gov.tr:238284</dc:identifier>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>http://www.opendefinition.org/licenses/cc-by</dc:rights>
  <dc:source>JOURNAL OF STRUCTURAL GEOLOGY 145</dc:source>
  <dc:title>Active tectonics and kinematics of Fethiye-G &amp; ouml;cek Bay, SW Turkey: Insight about the eastern edge of Pliny-Strabo Trenches</dc:title>
  <dc:type>info:eu-repo/semantics/article</dc:type>
  <dc:type>publication-article</dc:type>
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