KUZEYBATI İRAN İÇİN YAPI SINIRI ANALİZİ UYGULAMALARI

Yıl 2017, , 533 - 536, 18.12.2017

Sanli Ranjıtekantapeh Ezgi Erbek M. Nuri Dolmaz

https://doi.org/10.21923/jesd.329310

Öz

İran’ın Kuzeybatısı, Alp Himalaya çarpışma bölgesinde; kuzeyde
Kafkaslar, güneyde Zagros Bindirme Kuşağı arasında yer almakta ve  aktif bir tektonik yapıya sahiptir. Bölgedeki
yapıların tektonik ve jeolojik özelliklerini inceleyerek yapı sınırlarının
belirlenmesi amacıyla bölgeye ait toplam alan manyetik verileri kullanılarak
Analitik sinyal ve yatay türev analitik sinyal görüntü haritaları oluşturulmuştur.
Oluşturulan haritalar üzerinde bölge için önemli olan çöküntü alanı olarak
gözlenen Urmia gölü, sabalan volkanı ve dağ kuşakları gibi yapıların sınırları
belirlenmiş ve Sabalan Volkanı’ nın yaklaşık olarak 90km² lik bir
alanı kapladığı tespit edilmiştir.

Anahtar Kelimeler

KB İran, Analitik sinyal, Yatay türev

BOUNDARY ANALYSIS APPLICATIONS FOR NORTWEST IRAN

Öz

The Northwest of Iran, is located in the Alpine
Himalayan collision zone; where there is an active seismic zone between the
Caucasus in the north and the Zagros Overthrust Zone in the south and it has
active tevtonic structure. In order to determine the tectonic and geological
properties of the structures in the study area, analytic signal and horizontal
gradient analytic signal method were generaterd using total magnetic field data
belonging to the region. Boundaries of structure like
Urmia Lake, which is observed as a collapse area, Sabalan Volcano and mountain
belt were determined and it has been 
identified that Sabalan Volcano covers approximately 90 km²    

Anahtar Kelimeler

NW Iran, Analytic Signal, Horizontal Gradient, Sabalan Volcano

Kaynakça

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