DOI: 10.1007/s00531-014-1083-9
Scopus记录号: 2-s2.0-84925532920
论文题名: Tectonostratigraphic evolution of the basins on the southern branch of the North Anatolian Fault System in the SE Marmara Region, Turkey
作者: Doğan B. ; Tüysüz O. ; Şanlı F.B.
刊名: International Journal of Earth Sciences
ISSN: 14373254
出版年: 2014
卷: 104, 期: 2 起始页码: 389
结束页码: 418
语种: 英语
英文关键词: Lazy Z-shaped pull-apart basin
; Lithostratigraphy
; Right-lateral strike-slip fault
; Sakarya River
; Southern branch of the North Anatolian Fault System
英文摘要: The lithostratigraphy of the Mekece–Iznik Corridor, the Geyve–Pamukova, and the Iznik basins on the southern branch of the North Anatolian Fault System (NAFS-SB) was investigated in detail. The intra-basin deposits carried by Sakarya River and the drainage systems in the northern and southern elevated blocks of the Iznik and Geyve–Pamukova Basins have been classified based on their lithofacies characteristics. The Geyve–Pamukova basin, which has developed with a NNE–SSW-trending transtensional strain, was formed as a lazy Z-shaped and releasing bend or pure strike-slip, pull-apart basin that is related to simple-shear, right-lateral strike-slip faulting. The Iznik basin was formed by a right-lateral strike-slip faulting kinematics and NNE–SSW-trending transtension as a result of the step-over of the northeast-trending Dırazali fault from the southern edge to the NW-trending Gürle fault, and the western step-over of this fault to the E–W-trending Umurbey fault. This strike-slip setting is also supported by the NW–SE-trending right-lateral oblique normal Orhangazi fault on the northern edge of the basin. According to this, the Iznik basin can be described as a more advanced stage of a large-scale, pull-apart basin compared with a lazy Z-shaped and releasing bend or transtensional strain. Furthermore, it is defined as the former stage of an extreme or rhomboid-type transtensional pull-apart basin. © 2014, Springer-Verlag Berlin Heidelberg. URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84925532920&doi=10.1007%2fs00531-014-1083-9&partnerID=40&md5=0cff103a38727578e2e3a4a61278126e
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/70338
Appears in Collections: 影响、适应和脆弱性 气候减缓与适应
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作者单位: Deparment of Geological Engineering, University of Kocaeli, Umuttepe Campus, Izmit, Kocaeli, Turkey; ITU, Eurasia Institute of Earth Sciences, Maslak, Istanbul, Turkey; Department of Geomatic Engineering, Yıldız Technical University, Davutpasa Campus, Esenler, Istanbul, Turkey
Recommended Citation:
Doğan B.,Tüysüz O.,Şanlı F.B.. Tectonostratigraphic evolution of the basins on the southern branch of the North Anatolian Fault System in the SE Marmara Region, Turkey[J]. International Journal of Earth Sciences,2014-01-01,104(2)