Başkale Fault Zone is
located between Şemdinli-Yüksekova fault zone in southeast Turkey and
Guilato–Siahcheshmeh–Khoy fault system in southeast Iran. The fault zone
started from Yavuzlar town to Işıklar village in southwest. BFZ is composed of
three different segments which have directions with varying N75°E to N 80°E.
The offset streams, fault controlled drainage system such as Çığılsuyu stream,
alluvial fans which line up parallel to the fault and have deformation
structure, fault straight, Plio-Quaternary volcanic rocks and volcanic
structures, ridge travertines which continues their formations today indicate
that BFZ is active as morphotectonic. The objective of the investigation is to
determine the effect of Başkale Fault Zone on morphotectonic evolution of the
region. With this aim, morphometric indices such hypsometric integral, drainage
basin asymmetry, the ratio between the width and the height of valley and crimp
in front of the mountain were produced with Digital Elevation Model of study
area and were explained with their meaning. Depending on the results of
morphometric models, it appears that the region has young topography and
activelyrises. It was concluded that the rate of topographies rise in the
region increased from east to west and typically rates were greater than of 0.5
mm in year.
Başkale Fault Zone Morphotectonic geomorphic indices uplift rates Eastern Anatolia
Birincil Dil | İngilizce |
---|---|
Konular | Mühendislik |
Bölüm | Makaleler |
Yazarlar | |
Yayımlanma Tarihi | 3 Aralık 2017 |
Yayımlandığı Sayı | Yıl 2017 Cilt: 155 Sayı: 155 |
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