TY - JOUR TT - BOUNDARY ANALYSIS APPLICATIONS FOR NORTWEST IRAN AU - Erbek, Ezgi AU - Ranjıtekantapeh, Sanli AU - Dolmaz, M. Nuri PY - 2017 DA - December Y2 - 2017 DO - 10.21923/jesd.329310 JF - Mühendislik Bilimleri ve Tasarım Dergisi JO - MBTD PB - Süleyman Demirel Üniversitesi WT - DergiPark SN - 1308-6693 SP - 533 EP - 536 VL - 5 IS - 3 KW - KB İran KW - Analitik sinyal KW - Yatay türev N2 - The Northwest of Iran, is located in the AlpineHimalayan collision zone; where there is an active seismic zone between theCaucasus in the north and the Zagros Overthrust Zone in the south and it hasactive tevtonic structure. In order to determine the tectonic and geologicalproperties of the structures in the study area, analytic signal and horizontalgradient analytic signal method were generaterd using total magnetic field databelonging to the region. Boundaries of structure likeUrmia Lake, which is observed as a collapse area, Sabalan Volcano and mountainbelt were determined and it has beenidentified that Sabalan Volcano covers approximately 90 km2 CR - 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. CR - Alavi, M., 1991. Tectonic Map of The Middle East. Geological Survey of Iran, Tehran. CR - 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. CR - Bournas, N. and Baker, H. A. 2001. Interpretation of magnetic anomalies using the horizontal gradient analytic signal. Annali Di Geofisica, 44; 505-526. CR - 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. CR - Eftekharnejad, J., 1976. Report of Geological map of Tabriz-Poldasht. 1:100,000 series. Geological Survey of Iran. CR - Emami, M.H., Asadian, O., Amini-Fazl, A., Khodabandeh, A., 1993. Geological Map of Qarachaman Quadrant. Geological Survey of Iran. CR - Ghanbari, E., 2001. Geothermal Studies in The Savalan and Other Volcano Fields in Azerbaijian. ISES Solar World Congress. 957–960. CR - 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. CR - Nabavi, M.H., 1976. An Iintroduction to The Geology of Iran, Geological Survey of Iran, Report No. 38, In Farsi. CR - 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. CR - Nabighian, M.N. 1974. Additional Comments on The Analytic Signal of Two Dimensional Magnetic Bodies with Polygonal Cross-section, Geophysics, 39, 85-92. CR - 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. CR - Stocklin, J., 1968. Structural History and Tectonics of Iran, A review. AAPG Bulletin, 52, 7, 1229-1258. CR - Stocklin, J., ve Nabavi, M.H., 1973. Tectonic map of Iran (1/2,500,000). Ministry of Mines and Metals, Geological Survey of Iran. CR - 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. UR - https://doi.org/10.21923/jesd.329310 L1 - https://dergipark.org.tr/tr/download/article-file/385923 ER -