NEOTECTONIC DEVELOPMENT OF THE ÇAMELI BASIN, SOUTHWESTERN ANATOLIA, TURKEY
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dc.contributor.author | Alçiçek M.C. | |
dc.contributor.author | Özkul M. | |
dc.contributor.author | Ten Veen J.H. | |
dc.date.accessioned | 2024-12-02T06:55:48Z | |
dc.date.available | 2024-12-02T06:55:48Z | |
dc.date.issued | 2006 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=14593493 | |
dc.identifier.citation | Geological Society Special Publication, 2006, 260, 260. С. 5, 591-611 | |
dc.identifier.issn | 0305-8719 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/46744 | |
dc.description.abstract | This study of the Çameli Basin presents a detailed basin evolution combined with structural analysis and provides the first detailed time-stratigraphic framework for the neotectonic development of Neogene grabens along the Fethiye-Burdur Fault Zone in southwestern Anatolia. During the Early Tortonian, the Çameli Basin was established as a broad fault-bounded fluviolacustrine basin that experienced NW-SE extension. By Mid-Pliocene time, continued NW-SE extension resulted in the formation of a new intrabasinal fault zone that split the basin longitudinally into two compartments. The development of a new generation of normal faults further split the basin into four narrow half-graben compartments at the end of the Late Pliocene. Structural analysis of basin-bounding and intrabasinal faults related to this three-stage basin development shows that NW-SE extension apparently persisted from Late Miocene to early Quaternary time. The youngest (i.e. Holocene), deformation is characterized by dextral shear along NE-SW-trending strike-slip faults and continuing NW-SE extension. The Late Miocene foundering of the basin was related to extension in the northerly hinterland zone of the still-emplacing Lycian nappes, whereas outward growth of the Hellenic Arc in response to the westward Anatolian extrusion is the main cause for NW-SE extension from the Pliocene onward. Dextral strike-slip faulting is localized and is associated with the activity of NW-SE-trending faults that accommodated NE-SW extension. The simultaneous activity of these faults suggests the existence of biaxial extensional tectonics, as initially proposed for the Burdur-Dinar area. Sinistral strike-slip faulting, continuing along the eastern Hellenic Arc, penetrated the southernmost part of Turkey but has not yet reached the Çameli Basin area. Our biostratigraphically well-constrained tectonosedimentary model for the evolution of the Çameli Basin provides a reliable time-stratigraphic framework for NE-SW extension in the 'Fethiye-Burdur Fault Zone' of SW Anatolia. We believe that this fault zone represents a broad zone of isolated or interconnected NE-SW-trending basins that formed under prevailing NW-SE extension, rather than being a significant strike-slip fault zone. © The Geological Society of London 2006. | |
dc.subject | Holocene | |
dc.subject | Pliocene | |
dc.subject | Tortonian | |
dc.title | NEOTECTONIC DEVELOPMENT OF THE ÇAMELI BASIN, SOUTHWESTERN ANATOLIA, TURKEY | |
dc.type | Статья | |
dc.identifier.doi | 10.1144/GSL.SP.2006.260.01.25 | |
dc.subject.age | Cenozoic::Quaternary::Holocene | |
dc.subject.age | Кайнозой::Четвертичная::Голоцен | |
dc.subject.age | Cenozoic::Neogene::Pliocene | |
dc.subject.age | Кайнозой::Неоген::Плиоцен | |
dc.subject.age | Cenozoic::Neogene::Miocene::Tortonian | |
dc.subject.age | Кайнозой::Неоген::Миоцен::Тортонский |
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