2016
DOI: 10.5152/ucd.2014.2871
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Turkish surgeons’ experiences and perception about single-incision laparoscopic surgery

Abstract: Objective: We aimed to show Turkish surgeons' current status of experience and perception about single-incision laparoscopic surgery. Material and Methods:The experience and perception of general surgeons, who were members of the Turkish Surgical Association (3.5%, 116/3312), about single-incision laparoscopic surgery were analyzed according to demographic characteristics and a self-report questionnaire with the following four domains: surgeons' perception regarding the performance of single-incision laparosco… Show more

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Cited by 2 publications
(3 citation statements)
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“…The lower Triassic-Campanian Munzur Limestone constitutes the eastern section of the Mesozoic 'Calcareous Axis' of the Tauride Platform (Ricou, 1980;Özgül, 1981), and consists mainly of neritic shelf carbonates. The late Cretaceous-Paleocene turbiditic sedimentary rocks resting unconformably over the ophiolite constrain its emplacement age as the late Cretaceous (Yılmaz, 1985;Yılmaz et al, 1990;Aktimur et al, 1995). Following its emplacement, the Refahiye ophiolite was thrust back onto the Permo-Triassic metamorphic rocks of the Sakarya Continent in the north as a result of continental collision between Eurasia and the Anatolide-Tauride platform (Fig.…”
Section: Geology Of the Refahiye Ophiolitementioning
confidence: 99%
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“…The lower Triassic-Campanian Munzur Limestone constitutes the eastern section of the Mesozoic 'Calcareous Axis' of the Tauride Platform (Ricou, 1980;Özgül, 1981), and consists mainly of neritic shelf carbonates. The late Cretaceous-Paleocene turbiditic sedimentary rocks resting unconformably over the ophiolite constrain its emplacement age as the late Cretaceous (Yılmaz, 1985;Yılmaz et al, 1990;Aktimur et al, 1995). Following its emplacement, the Refahiye ophiolite was thrust back onto the Permo-Triassic metamorphic rocks of the Sakarya Continent in the north as a result of continental collision between Eurasia and the Anatolide-Tauride platform (Fig.…”
Section: Geology Of the Refahiye Ophiolitementioning
confidence: 99%
“…The residues after high degrees of melting are commonly highly depleted in incompatible elements, compared to the low-degree melting residues, in both bulk and mineral chemistry. Aktimur et al, 1995;Özen et al, 2008;Sarifakioglu et al, 2009), showing the peridotite sample locations. Inset map displays the major tectonic belts (Dinter, 1998) and the distribution of major ophiolite complexes in Turkey (Dilek and Furnes, 2009).…”
Section: Introductionmentioning
confidence: 99%
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