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KUZEYBATI İRAN İÇİN YAPI SINIRI ANALİZİ UYGULAMALARI

Yıl 2017, Cilt: 5 Sayı: 3, 533 - 536, 18.12.2017
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.

Kaynakça

  • Abdollahi, S., Mohajjel, M., Salagi, A., ve Tag-hipour, K., 2012. Compressional termi-nation of North Tabriz Fault in Bozkush mountains, 30th GSI congress, Iran, 7.
  • Alavi, M., 1991. Tectonic Map of The Middle East. Geological Survey of Iran, Tehran.
  • Barbarian, M., ve Arshadi, S. S., 1976. On The evidence of the youngesy activity of the North Tabriz Fault and The seismity Of Tabriz city. GIS NO 39.
  • Bournas, N. and Baker, H. A. 2001. Interpretation of magnetic anomalies using the horizontal gradient analytic signal. Annali Di Geofisica, 44; 505-526.
  • Chiu H Y, Chung S L, Zarrinkoub M H, Mohammadi S S, Khatib M M,Iizuka Y. 2013. Zircon U-Pb Age Constraints from Iran on The Magmatic Evolution Related to Neotethyan Subduction and Zagros Orogeny. Lithos, 162-163: 70–87.
  • Eftekharnejad, J., 1976. Report of Geological map of Tabriz-Poldasht. 1:100,000 series. Geological Survey of Iran.
  • Emami, M.H., Asadian, O., Amini-Fazl, A., Khodabandeh, A., 1993. Geological Map of Qarachaman Quadrant. Geological Survey of Iran.
  • Ghanbari, E., 2001. Geothermal Studies in The Savalan and Other Volcano Fields in Azerbaijian. ISES Solar World Congress. 957–960.
  • Manaman, N.S., Shomali, H., Koyi, H., 2011. New Constraints on Upper-Mantle S-Velocity Structure and Crustal Thickness of The Iranian Plateau Using Partitioned Waveform İnversion. Geophysical Journal International, 184, 247–267.
  • Nabavi, M.H., 1976. An Iintroduction to The Geology of Iran, Geological Survey of Iran, Report No. 38, In Farsi.
  • Nabighian, M.N., 1972. The Analytic Signal of Two-Dimensional Magnetic Bodies with Polygonal Cross-section: Its Properties and Use for Automated Anomaly İnterpretation. Geophysics, 37, 507–517.
  • Nabighian, M.N. 1974. Additional Comments on The Analytic Signal of Two Dimensional Magnetic Bodies with Polygonal Cross-section, Geophysics, 39, 85-92.
  • Roest, W.R., Verhoef, J., Pilkington, M., 1992. Magnetic Interpretation Using the 3-D Analytic Signal. Geophysics, 57, 116-25. Saber, R., Işık, V,. Çağlayan, A., 2013. Geology of The North Bozgush Fault Zone and Its Tectonic Significance, NW Iran, Yerbilimleri 32, 2, 83-100.
  • Stocklin, J., 1968. Structural History and Tectonics of Iran, A review. AAPG Bulletin, 52, 7, 1229-1258.
  • Stocklin, J., ve Nabavi, M.H., 1973. Tectonic map of Iran (1/2,500,000). Ministry of Mines and Metals, Geological Survey of Iran.
  • Şengör, A.M.C., 1990. A New Model for The Late Paleozoic–Mesozoic Tectonic Evolution of Iran and Implications for Oman. The Geology and Tectonics of the Oman region. Geol. Soc. Spec. Publ. London, 797–831.

BOUNDARY ANALYSIS APPLICATIONS FOR NORTWEST IRAN

Yıl 2017, Cilt: 5 Sayı: 3, 533 - 536, 18.12.2017
https://doi.org/10.21923/jesd.329310

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
    

Kaynakça

  • Abdollahi, S., Mohajjel, M., Salagi, A., ve Tag-hipour, K., 2012. Compressional termi-nation of North Tabriz Fault in Bozkush mountains, 30th GSI congress, Iran, 7.
  • Alavi, M., 1991. Tectonic Map of The Middle East. Geological Survey of Iran, Tehran.
  • Barbarian, M., ve Arshadi, S. S., 1976. On The evidence of the youngesy activity of the North Tabriz Fault and The seismity Of Tabriz city. GIS NO 39.
  • Bournas, N. and Baker, H. A. 2001. Interpretation of magnetic anomalies using the horizontal gradient analytic signal. Annali Di Geofisica, 44; 505-526.
  • Chiu H Y, Chung S L, Zarrinkoub M H, Mohammadi S S, Khatib M M,Iizuka Y. 2013. Zircon U-Pb Age Constraints from Iran on The Magmatic Evolution Related to Neotethyan Subduction and Zagros Orogeny. Lithos, 162-163: 70–87.
  • Eftekharnejad, J., 1976. Report of Geological map of Tabriz-Poldasht. 1:100,000 series. Geological Survey of Iran.
  • Emami, M.H., Asadian, O., Amini-Fazl, A., Khodabandeh, A., 1993. Geological Map of Qarachaman Quadrant. Geological Survey of Iran.
  • Ghanbari, E., 2001. Geothermal Studies in The Savalan and Other Volcano Fields in Azerbaijian. ISES Solar World Congress. 957–960.
  • Manaman, N.S., Shomali, H., Koyi, H., 2011. New Constraints on Upper-Mantle S-Velocity Structure and Crustal Thickness of The Iranian Plateau Using Partitioned Waveform İnversion. Geophysical Journal International, 184, 247–267.
  • Nabavi, M.H., 1976. An Iintroduction to The Geology of Iran, Geological Survey of Iran, Report No. 38, In Farsi.
  • Nabighian, M.N., 1972. The Analytic Signal of Two-Dimensional Magnetic Bodies with Polygonal Cross-section: Its Properties and Use for Automated Anomaly İnterpretation. Geophysics, 37, 507–517.
  • Nabighian, M.N. 1974. Additional Comments on The Analytic Signal of Two Dimensional Magnetic Bodies with Polygonal Cross-section, Geophysics, 39, 85-92.
  • Roest, W.R., Verhoef, J., Pilkington, M., 1992. Magnetic Interpretation Using the 3-D Analytic Signal. Geophysics, 57, 116-25. Saber, R., Işık, V,. Çağlayan, A., 2013. Geology of The North Bozgush Fault Zone and Its Tectonic Significance, NW Iran, Yerbilimleri 32, 2, 83-100.
  • Stocklin, J., 1968. Structural History and Tectonics of Iran, A review. AAPG Bulletin, 52, 7, 1229-1258.
  • Stocklin, J., ve Nabavi, M.H., 1973. Tectonic map of Iran (1/2,500,000). Ministry of Mines and Metals, Geological Survey of Iran.
  • Şengör, A.M.C., 1990. A New Model for The Late Paleozoic–Mesozoic Tectonic Evolution of Iran and Implications for Oman. The Geology and Tectonics of the Oman region. Geol. Soc. Spec. Publ. London, 797–831.
Toplam 16 adet kaynakça vardır.

Ayrıntılar

Konular Mühendislik
Bölüm Araştırma Makaleleri \ Research Articles
Yazarlar

Sanli Ranjıtekantapeh Bu kişi benim 0000-0002-1902-1587

Ezgi Erbek Bu kişi benim 0000-0003-4627-8932

M. Nuri Dolmaz Bu kişi benim 0000-0002-9185-9835

Yayımlanma Tarihi 18 Aralık 2017
Gönderilme Tarihi 18 Temmuz 2017
Kabul Tarihi 2 Kasım 2017
Yayımlandığı Sayı Yıl 2017 Cilt: 5 Sayı: 3

Kaynak Göster

APA Ranjıtekantapeh, S., Erbek, E., & Dolmaz, M. N. (2017). KUZEYBATI İRAN İÇİN YAPI SINIRI ANALİZİ UYGULAMALARI. Mühendislik Bilimleri Ve Tasarım Dergisi, 5(3), 533-536. https://doi.org/10.21923/jesd.329310