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Publikováno v:
Tectonophysics. 762:121-143
The Anaximander Mountains and the Rhodes Basin at the junction of Cyprus and Hellenic arcs are one of the tectonically most complex regions in the eastern Mediterranean. Harmonically-tilted Messinian and the uppermost Messinian–Pliocene successions
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cdd5d15c5a406620a40e69c515e511b6
https://doi.org/10.1016/j.tecto.2019.04.031
https://doi.org/10.1016/j.tecto.2019.04.031
Publikováno v:
Hand surgeryrehabilitation. 40(6)
The superficial location of critical structures, including tendons, nerves and vessels, in the volar surface of the wrist makes them vulnerable to penetrating trauma. Extensive injuries to these structures are described as “spaghetti wrist”. The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::848aba71e30d10b290dae82bb494f7df
https://pubmed.ncbi.nlm.nih.gov/34403786
https://pubmed.ncbi.nlm.nih.gov/34403786
Publikováno v:
Marine and Petroleum Geology. 136:105451
A dense grid of high-resolution multichannel seismic reflection profiles are used to delineate the stratigraphic and structural architecture of the Anamur–Kormakiti zone which separates the Outer Cilicia Basin from the eastern Antalya Basin. The da
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::16cde1130443e27b81be560b1abc5ef1
https://doi.org/10.1016/j.marpetgeo.2021.105451
https://doi.org/10.1016/j.marpetgeo.2021.105451
Publikováno v:
Marine Geology. 434:106441
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dbd4c1725f9dae2b215233a695d2d7b2
https://doi.org/10.1016/j.margeo.2021.106441
https://doi.org/10.1016/j.margeo.2021.106441
Publikováno v:
Marine Geology. 380:113-137
The chronology of an abandoned Holocene delta lobe (present water depth ~40–70 m) on the northeastern shelf of the Marmara Sea south of the Strait of Bosphorus was revised from the early Holocene (~11.0–9.7 cal ka) to the middle Holocene (6.65–
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::248eafbc54fa759fe9312a8b18639d8d
https://doi.org/10.1016/j.margeo.2016.07.003
https://doi.org/10.1016/j.margeo.2016.07.003
Publikováno v:
Marine Geology. 420:106092
An extensive grid of high-resolution Huntec deep-tow seismic reflection profiles (~9150 line-km), complemented by 72 gravity cores and 25 piston cores reveals that the sedimentary architecture of the southwestern Black Sea above a prominent shelf-cro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2fc1da6828dbfe48679d5ce5c30014b8
https://doi.org/10.1016/j.margeo.2019.106092
https://doi.org/10.1016/j.margeo.2019.106092
Publikováno v:
Tectonophysics. 664:5-13
• This confirms our previous suggestions that the Fethiye-Burdur Fault Zone is a 75-90 km-wide, left-lateral, fault zone.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::af67f822df42f204bfe5ffdce588c87b
https://doi.org/10.1016/j.tecto.2015.04.002
https://doi.org/10.1016/j.tecto.2015.04.002
Publikováno v:
Tectonophysics. 635:80-99
The Hellenic and Cyprus Arcs, that mark the convergent boundary of the African and Aegean-Anatolian plates, are offset along a subduction transform edge propagator ('STEP') fault running NE-SW along the Pliny and Strabo Trenches. The continuation of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4c5f6ef866af2d30916289711318ddf8
https://doi.org/10.1016/j.tecto.2014.05.002
https://doi.org/10.1016/j.tecto.2014.05.002
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 533:109227
Oxygen and carbon isotopes and trace-element/Ca ratios are presented for the valves of benthic ostracods Palmoconcha agilis and Loxoconcha lepida extracted from two composite sediment cores from the Black Sea shelf. The two cores together provide a c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::47e8c17f515ba25ce7bdc15fd3c9ecb1
https://doi.org/10.1016/j.palaeo.2019.05.049
https://doi.org/10.1016/j.palaeo.2019.05.049