Evaluation of tectonic structure of İskenderun Basin (Turkey) using steerable filters
In this paper, we demonstrate the effectiveness of steerable filters as a method of delineating the boundaries of subsurface geological structures. Steerable filters, generally used for edge detection on 2-D images, have the properties of band pass filters with certain directions and are applied to...
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Published in | Marine geophysical researches Vol. 27; no. 4; pp. 225 - 239 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
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Springer Nature B.V
01.01.2006
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Abstract | In this paper, we demonstrate the effectiveness of steerable filters as a method of delineating the boundaries of subsurface geological structures. Steerable filters, generally used for edge detection on 2-D images, have the properties of band pass filters with certain directions and are applied to many image processing problems. We first tested the method on synthetic data and then applied it to the aeromagnetic data of Iskenderun Basin and adjacent areas. Iskenderun Basin is located in the Northeastern Mediterranean where African-Arabian and Anatolian plates are actively interacting. The basin fill records a complex tectonic evolution since the Early Miocene, involving ophiolite emplacement, diachronous collision of Eurasian and Arabian plates and subsequent tectonic escape related structures and associated basin formation. Geophysical investigations of the tectonic framework of Iskenderun Basin of Turkey provide important insights on the regional tectonics of the Eastern Mediterranean and Middle East. In this study we show geological structures, which are responsible for the magnetic anomalies in Iskenderun Basin and enlighten the structural setting of the Northeastern Mediterranean triple junction using steerable filters. We obtained a magnetic anomaly map of the region from the General Directorate of Mineral Research and Exploration as raw data and then evaluated this by steerable filters. We determined the magnetic anomaly boundaries for Iskenderun Basin by using various types of steerable filters and correlated these to drilling data and seismic profiles from the Turkish Petroleum Corporation. The result of the steerable filter analysis was a clarified aeromagnetic anomaly map of Iskenderun Basin. The tectonic structure of Iskenderun Basin is divided into regions by an N-S trending oblique-slip fault defined by the steerable filter outputs. We propose a new tectonic structure model of Iskenderun Basin and modify the direction of the East Anatolian Fault Zone. In our model, East Anatolian Fault Zone cross-cuts the basin as a narrow fault zone and continues towards the Cyprus arc.[PUBLICATION ABSTRACT] |
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AbstractList | In this paper, we demonstrate the effectiveness of steerable filters as a method of delineating the boundaries of subsurface geological structures. Steerable filters, generally used for edge detection on 2-D images, have the properties of band pass filters with certain directions and are applied to many image processing problems. We first tested the method on synthetic data and then applied it to the aeromagnetic data of Iskenderun Basin and adjacent areas.Iskenderun Basin is located in the Northeastern Mediterranean where African-Arabian and Anatolian plates are actively interacting. The basin fill records a complex tectonic evolution since the Early Miocene, involving ophiolite emplacement, diachronous collision of Eurasian and Arabian plates and subsequent tectonic escape related structures and associated basin formation. Geophysical investigations of the tectonic framework of Iskenderun Basin of Turkey provide important insights on the regional tectonics of the Eastern Mediterranean and Middle East. In this study we show geological structures, which are responsible for the magnetic anomalies in Iskenderun Basin and enlighten the structural setting of the Northeastern Mediterranean triple junction using steerable filters. We obtained a magnetic anomaly map of the region from the General Directorate of Mineral Research and Exploration as raw data and then evaluated this by steerable filters. We determined the magnetic anomaly boundaries for Iskenderun Basin by using various types of steerable filters and correlated these to drilling data and seismic profiles from the Turkish Petroleum Corporation. The result of the steerable filter analysis was a clarified aeromagnetic anomaly map of Iskenderun Basin. The tectonic structure of Iskenderun Basin is divided into regions by an N-S trending oblique-slip fault defined by the steerable filter outputs. We propose a new tectonic structure model of Iskenderun Basin and modify the direction of the East Anatolian Fault Zone. In our model, East Anatolian Fault Zone cross-cuts the basin as a narrow fault zone and continues towards the Cyprus arc. In this paper, we demonstrate the effectiveness of steerable filters as a method of delineating the boundaries of subsurface geological structures. Steerable filters, generally used for edge detection on 2-D images, have the properties of band pass filters with certain directions and are applied to many image processing problems. We first tested the method on synthetic data and then applied it to the aeromagnetic data of Iskenderun Basin and adjacent areas. Iskenderun Basin is located in the Northeastern Mediterranean where African-Arabian and Anatolian plates are actively interacting. The basin fill records a complex tectonic evolution since the Early Miocene, involving ophiolite emplacement, diachronous collision of Eurasian and Arabian plates and subsequent tectonic escape related structures and associated basin formation. Geophysical investigations of the tectonic framework of Iskenderun Basin of Turkey provide important insights on the regional tectonics of the Eastern Mediterranean and Middle East. In this study we show geological structures, which are responsible for the magnetic anomalies in Iskenderun Basin and enlighten the structural setting of the Northeastern Mediterranean triple junction using steerable filters. We obtained a magnetic anomaly map of the region from the General Directorate of Mineral Research and Exploration as raw data and then evaluated this by steerable filters. We determined the magnetic anomaly boundaries for Iskenderun Basin by using various types of steerable filters and correlated these to drilling data and seismic profiles from the Turkish Petroleum Corporation. The result of the steerable filter analysis was a clarified aeromagnetic anomaly map of Iskenderun Basin. The tectonic structure of Iskenderun Basin is divided into regions by an N-S trending oblique-slip fault defined by the steerable filter outputs. We propose a new tectonic structure model of Iskenderun Basin and modify the direction of the East Anatolian Fault Zone. In our model, East Anatolian Fault Zone cross-cuts the basin as a narrow fault zone and continues towards the Cyprus arc.[PUBLICATION ABSTRACT] |
Author | Albora, A. Muhittin Uçan, Osman N. Sayın, Nurdan |
Author_xml | – sequence: 1 givenname: A. Muhittin surname: Albora fullname: Albora, A. Muhittin – sequence: 2 givenname: Nurdan surname: Sayın fullname: Sayın, Nurdan – sequence: 3 givenname: Osman N. surname: Uçan fullname: Uçan, Osman N. |
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CitedBy_id | crossref_primary_10_1007_s00024_018_1771_7 crossref_primary_10_1134_S0016702911110097 crossref_primary_10_1016_j_jafrearsci_2022_104780 crossref_primary_10_1016_j_lithos_2018_06_008 crossref_primary_10_1007_s00024_017_1604_0 crossref_primary_10_1016_j_chemer_2018_08_001 crossref_primary_10_1016_j_jafrearsci_2020_103828 crossref_primary_10_1007_s12665_019_8435_5 crossref_primary_10_1016_j_geothermics_2017_06_016 |
Cites_doi | 10.1016/S1367-9120(03)00062-2 10.1016/S0377-0273(98)00046-8 10.1016/0040-1951(90)90367-H 10.1038/226239a0 10.1190/1.1442197 10.1111/j.1365-246X.1984.tb01931.x 10.1002/1099-1034(200004/06)35:2<53::AID-GJ837>3.0.CO;2-6 10.1029/94JB00335 10.1111/j.1365-246X.1972.tb02351.x 10.1016/j.margeo.2005.03.010 10.1016/j.tecto.2004.04.005 10.2110/pec.85.37.0227 10.1109/ISCAS.1995.523803 10.1130/0016-7606(1999)111<1192:SAPOTO>2.3.CO;2 10.1111/j.1365-246X.1991.tb06328.x 10.1144/gsjgs.153.5.0729 10.1016/0040-1951(90)90039-B 10.1016/j.tecto.2004.07.014 10.1029/JB094iB04p04007 10.1080/09853111.2001.11432432 10.1029/TC006i006p00687 10.1016/j.jseaes.2005.02.004 10.1109/34.93808 10.1016/0040-1951(81)90275-4 10.1144/gsjgs.154.5.0757 10.1016/0191-8141(87)90091-5 10.1785/0120020153 10.1016/0040-1951(88)90020-0 10.1016/0040-1951(92)90265-8 10.1016/j.crte.2003.10.016 |
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Title | Evaluation of tectonic structure of İskenderun Basin (Turkey) using steerable filters |
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