Results 1 to 10 of about 18,000 (82)
Lithostratigraphy and planktonic foraminifera of the uppermost Cretaceous-Upper Paleocene strata of the Tavas nappe of the Lycian nappes (SW Turkey) [PDF]
Geologia Croatica, 2017 The Lycian nappes lying on top of the para–autochthonous metamorphosed Menderes and unmetamorphosed Bey Dağları successions in SW Anatolia belong to the Tauride segment of the Anatolide–Tauride Block.
Bilal Sari
doaj +8 more sources
Lithostratigraphy and Sedimentological Characteristics of the Calciturbidites of the Babadağ Formation-Tavas Nappe (SW Turkey) [PDF]
Geologia Croatica, 2021 The Lycian Nappes contain slices of ophiolites and sedimentary rocks of various ages that crop out in SW Turkey. They evolved and were emplaced under the effect of the Late Cretaceous-Miocene compressional regime. The Tavas Nappe is part of the Lycian Nappes and contains Jurassic-Eocene sediments.
Kore, Basiru Mohammed +3 more
semanticscholar +8 more sources
Occurrences of Chert in Jurassic-Cretaceous Calciturbidites (SWTurkey)
Open Geosciences, 2015 The Lycian Nappes, containing ophiolite andsedimentary rocks sequences, crop out in the southwestTurkey. The Tavas Nappe is a part of the Lycian Nappes.It includes the Lower Jurassic-Upper Cretaceous calciturbidites.Chert occurrences were observed in the
Gül Murat
doaj +5 more sources
Geologia Croatica, 2010 For the first time. a deep-water Lower Carbon iferous siliciclasticturbidite-olistostrome unit with many lydites (partly distally turbiditic) can be dated in the Incirbeleni Formation of the Tavas Nappe (Lycian nappes) in southwestern Turkey.
Heinz W. Kozur +2 more
doaj +2 more sources
, 2020 The Lycian Nappes are located within the southwestern part of Turkey, and areexposed between the Beydağları Autochthon, and the Menderes Massif. The LycianNappes are actually the northern peripherals of the Menderes Massif, and containUpper Cretaceous ophiolites and ophiolitic melange slices with sedimentary strataranging in age from Paleozoic to ...
openaire +1 more source
Journal of Asian Earth Sciences, 2015 Abstract Stratigraphic sections (Kizilca and Kizilca North) in the Tavas nappe, western Taurides, Turkey records the event of carbonate platform drowning in the western Tethyan realm. Our detailed biostratigraphic study of radiolarians and other microfossils places the important temporal constraints on this event and indicates that drowning occured ...
Havva Soycan +2 more
semanticscholar +3 more sources
International journal of earth sciences, 2013 WOS: 000325804900007Southwestern Turkey experienced a transition from crustal shortening to extension during Late Cenozoic, and evidence of this was recorded in four distinct basin types in the Mugla-Gokova Gulf region. During the Oligocene-Early Miocene,
Ö. F. Gürer +4 more
semanticscholar +2 more sources
Giant sheath-folded nappe stack demonstrates extreme subhorizontal shear strain in an Archean orogen
Geology, 2022 Giant sheath-folded nappes are associated with suture zones and emplacement of far-traveled allochthons in Phanerozoic orogens, demonstrating a rare but significant geologic phenomenon indicative of modern-style plate tectonics.
Yating Zhong, T. Kusky, Lu Wang
semanticscholar +1 more source
Tectonics, 2021 The E‐vergent Northern Apennines formed by Oligocene‐Miocene convergence and westward subduction of Adria beneath Europe. Extension ensued in the Mid‐Late Miocene reflecting lower plate roll‐back and causing opening of the back‐arc Northern Tyrrhenian ...
E. Ryan +7 more
semanticscholar +1 more source
Late Palaeozoic extensional volcanism along the northern margin of Gondwana in southern Turkey: implications for Palaeotethyan development [PDF]
, 2021 The Late Palaeozoic-Early Mesozoic Tethyan development of the Eastern Mediterranean region remains debatable, especially in Turkey, where alternative northward and southward subduction hypotheses are proposed.
Parlak, Osman +2 more
core +1 more source