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dc.contributor.authorRobertson, Alastair H. F.
dc.contributor.authorUstaomer, Timur
dc.date.accessioned2021-03-03T20:49:18Z
dc.date.available2021-03-03T20:49:18Z
dc.identifier.citationRobertson A. H. F. , Ustaomer T., "Upper Palaeozoic subduction/accretion processes in the closure of Palaeotethys: Evidence from the Chios Melange (E Greece), the Karaburun Melange (W Turkey) and the Teke Dere Unit (SW Turkey)", SEDIMENTARY GEOLOGY, cilt.220, ss.29-59, 2009
dc.identifier.issn0037-0738
dc.identifier.othervv_1032021
dc.identifier.otherav_5c030f84-bdb2-418b-b2fc-326b52d5a5fc
dc.identifier.urihttp://hdl.handle.net/20.500.12627/64530
dc.identifier.urihttps://doi.org/10.1016/j.sedgeo.2009.06.005
dc.description.abstractDuring Late Palaeozoic time a wide ocean, known as Palaeotethys, separated the future Eurasian and African continents. This ocean closed in Europe in the west during the Variscan orogeny, whereas in Asia further east it remained open and evolved into the Mesozoic Tethys, only finally closing during Late Cretaceous-Early Cenozoic.
dc.language.isoeng
dc.subjectTemel Bilimler (SCI)
dc.subjectJeoloji Mühendisliği
dc.subjectMühendislik ve Teknoloji
dc.subjectJEOLOJİ
dc.subjectYerbilimleri
dc.titleUpper Palaeozoic subduction/accretion processes in the closure of Palaeotethys: Evidence from the Chios Melange (E Greece), the Karaburun Melange (W Turkey) and the Teke Dere Unit (SW Turkey)
dc.typeMakale
dc.relation.journalSEDIMENTARY GEOLOGY
dc.contributor.departmentUniversity Of Edinburgh , ,
dc.identifier.volume220
dc.identifier.startpage29
dc.identifier.endpage59
dc.contributor.firstauthorID41901


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