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GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Asia
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Kizilirmak River
Detailed drainage maps along the southern CAP (locations on Fig. 2B ): (A)...
(A) Topographic map of Turkey with an overlay of exposed Neogene sedimentar...
The slip history solution of Model II, which is calculated for the fault se...
Cross sections of key areas (locations on Fig. 2B ). Lower Zamantı: b-b*: ...
Fast Pliocene integration of the Central Anatolian Plateau drainage: Evidence, processes, and driving forces
The North Anatolian Shear Zone (NASZ: delimited by discontinuous lines) and...
Paleoenvironmental conditions and drainage evolution of the central Anatolian lake system (Turkey) during late Miocene to Pliocene surface uplift
Investigating the response of groundwater and streamflow to rainfall in a tropical catchment using non-parametric methods
Hamilton’s 1838 map of Central Anatolia ( Hamilton 1838b ), compared to a m...
A combined surface and groundwater storage project: the Elmadag dam (Turkey)
Organic geochemical characteristics of the bituminous Eocene units in the Çorum–Suluova Basin, Central Anatolia, Turkey
Abstract The Upper Kizilirmak Basin (UKB) of Tiirkiyecontains middle Eocene-Quaternary basin fill. This strike-slip basin in the central Anatolian Province isassociated with the Paleocene collision of the Arabianplate (Seng6r et aI., 1985). The UKB is surrounded(Figure 1) by the Akdag Mountains to the northwest (composed of Paleozoic metamorphics including marble) and the Caldag and Hinzir mountains to the south-southwest (composed of Paleozoicand Paleocene-Oligocene sedimentary rocks).The basin fill (Figure 2) contains a thick lower-middle Miocene sedimentary sequence called the Yenicubuk Formation, which is interpreted as alluvial to lacustrine in origin. This contribution focuses on the sedimentology of this formation in the area around Gemerek (Figure 2) within the UKB, where a50-km-long outcrop belt (Figure 1) trends northeast southwest.
Syneresis dependent shear strength parameters of sodium silicate grouted sands
A relict paleoseismic record of seven earthquakes between 2000 B.C. and 600 A.D. on the central North Anatolian fault at Elmacik, near Osmancik, Turkey
Syneresis effect on the permeability of chemically grouted sand
Relationships between the Sakarya Zone and the Ankara–Erzincan suture (central-northern Turkey): geological and petrographic data from the Ankara–Çankiri, Çorum and Amasya areas
Effects of Geo-Engineering Characteristics of the Soft Tuffs and Environmental Conditions on the Rock-Hewn Historical Structures at Zelve Open Air Museum, Cappadocia, Turkey
Spatio-temporal behaviour of continental transform faults: implications from the late Quaternary slip history of the North Anatolian Fault, Turkey
Abstract The Izmir–Ankara–Erzincan suture zone (IAESZ) in the Central and the Eastern Pontides comprises a stack of thrust sheets of mainly Late Cretaceous–Early Cenozoic age that are restored as: (1) a subduction–accretion complex; (2) a continental-margin magmatic arc, plus an associated forearc basin; (3) a back-arc basin and its mainly sedimentary fill. Northward thrusting affected all of the Late Cretaceous units during latest Cretaceous (Campanian–Maastrichtian) time. This was followed by regional southward thrusting to form the present thrust stack during Mid-Eocene time. Alternative tectonic models are considered in the light of sedimentary, igneous geochemical and structural evidence, and global comparisons. We infer that the Northern Neotethys was subducted northwards beneath the Eurasian active margin during the Late Cretaceous. Subduction was associated with the genesis of a magmatic arc and a related forearc basin. The subduction zone retreated oceanwards, associated with the opening of a back-arc basin along the Eurasian margin, floored by oceanic crust and overlain by mixed terrigenous and volcaniclastic deep-marine sediments. Ophiolite genesis in a continental margin back-arc setting is suggested by the presence of screens of basement-type metamorphic rocks within an ophiolite-related sheeted dyke complex in the Eastern Pontides. During the latest Cretaceous closure of the inferred back-arc basin resulted in northward emplacement of ophiolitic and related units onto the Eurasian margin, as well exposed in the Central Pontides. In addition, accretionary mélange, volcanic arc, forearc and ophiolitic units were emplaced southwards onto the Tauride continent, represented by the Munzur platform in the Eastern Pontides, also during latest Cretaceous time. This incipient (‘soft’) collision was followed by widespread Paleocene–Early Eocene deposition of Nummulitic shelf carbonates and coarse clastic sediments on deformed and emplaced accretionary mélange, arc and ophiolitic units. Final closure (‘hard collision’) of the Northern Neotethys occurred during the Mid-Eocene, resulting in large-scale southward imbrication, together with northward backthrusting in some areas. Suture tightening and Plio-Quaternary strike-slip ensued.