DOI: 10.1007/s00531-013-0909-1
Scopus记录号: 2-s2.0-84885940198
论文题名: Complex basin evolution in the Gökova Gulf region: Implications on the Late Cenozoic tectonics of southwest Turkey
作者: Gürer Ö.F. ; Sanǧu E. ; Özburan M. ; Gürbüz A. ; Sarica-Filoreau N.
刊名: International Journal of Earth Sciences
ISSN: 14373254
出版年: 2013
卷: 102, 期: 8 起始页码: 2199
结束页码: 2221
语种: 英语
英文关键词: Compression
; Extension
; Intermountain basin
; Nappe emplacement
; Neotectonic
; Piggyback basin
; Transpression
; Western Anatolia
Scopus关键词: basin evolution
; Cenozoic
; crustal shortening
; emplacement
; extensional tectonics
; Miocene
; nappe
; neotectonics
; normal fault
; piggyback basin
; Pliocene
; tectonic evolution
; tectonic setting
; transpression
; Aegean Sea
; Gokova Gulf
; Mediterranean Sea
; Menderes Massif
; Turkey
; Lycia
英文摘要: Southwestern 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 Muǧla-Gökova Gulf region. During the Oligocene-Early Miocene, the upper slices of the southerly moving Lycian Nappes turned into north-dipping normal faults due to the acceleration of gravity. The Kale-Tavas Basin developed as a piggyback basin along the fault plane on hanging wall blocks of these normal faults. During Middle Miocene, a shift had occurred from local extension to N-S compression/transpression, during which sediments in the Eskihisar-Ti{dotless}naz Basins were deposited in pull-apart regions of the Menderes Massif cover units, where nappe slices were already eroded. During the Late Miocene-Pliocene, a hiatus occurred from previous compressional/transpressional tectonism along intermountain basins and Yataǧan Basin fills were deposited on Menderes Massif, Lycian Nappes, and on top of Oligo-Miocene sediments. Plio-Quaternary marked the activation of N-S extension and the development of the E-W-trending Muǧla-Gökova Grabens, co-genetic equivalents of which are common throughout western Anatolia. Thus, the tectonic evolution of the western Anotolia during late Cenozoic was shifting from compressional to extensional with a relaxation period, suggesting a non-uniform evolution. © 2013 Springer-Verlag Berlin Heidelberg. URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84885940198&doi=10.1007%2fs00531-013-0909-1&partnerID=40&md5=dc3f68e9be4b0462a651786c727e6e82
Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/70487
Appears in Collections: 影响、适应和脆弱性 气候减缓与适应
There are no files associated with this item.
作者单位: Kocaeli Üniversitesi, Mühendislik Fakültesi, Jeoloji Mühendisliǧi Bölümü, Umuttepe Kampüsü, Kocaeli, Turkey; Dumlupinar Üniversitesi, Mühendislik Fakültesi, Jeoloji Mühendisliǧi Bölümü, Kütahya, Turkey; Ankara Üniversitesi, Mühendislik Fakültesi, Jeoloji Mühendisliǧi Bölümü, Ankara, Turkey; Niǧde Üniversitesi, Mühendislik Fakültesi, Jeoloji Mühendisliǧi Bölümü, Niǧde, Turkey; Prof. Dr. Hifzi Ozcan Cad. Adalet sitesi C Blok D.20 Kadik, Istanbul, Turkey
Recommended Citation:
Gürer Ö.F.,Sanǧu E.,Özburan M.,et al. Complex basin evolution in the Gökova Gulf region: Implications on the Late Cenozoic tectonics of southwest Turkey[J]. International Journal of Earth Sciences,2013-01-01,102(8)