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Tosun, Levent; Avsar, Ulas; Avsar, Ozgur; Dondurur, Derman; Kaymakci, Nuretdin
{ "DOI": "10.1016/j.jsg.2021.104287", "abstract": "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.", "author": [ { "family": "Tosun", "given": " Levent" }, { "family": "Avsar", "given": " Ulas" }, { "family": "Avsar", "given": " Ozgur" }, { "family": "Dondurur", "given": " Derman" }, { "family": "Kaymakci", "given": " Nuretdin" } ], "container_title": "JOURNAL OF STRUCTURAL GEOLOGY", "id": "238284", "issued": { "date-parts": [ [ 2021, 1, 1 ] ] }, "title": "Active tectonics and kinematics of Fethiye-G & ouml;cek Bay, SW Turkey: Insight about the eastern edge of Pliny-Strabo Trenches", "type": "article-journal", "volume": "145" }
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