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GEOPHYSICAL ANALYSIS AND MODELLING OF THE SİMAV BASIN, WESTERN ANATOLIA

Year 2014, , 119 - 135, 01.06.2014
https://doi.org/10.19111/bmre.81669

Abstract

The various data processing techniques, to illuminate the parameters of the geologicalstructure which are applied in gravity and magnetic potential field methods. Also edgedetection procedures are in data processing techniques. In this study, 2D, 3D, inversionand asta technique is one of the new edge detection procedures were applied to clarifycorrelation between the Simav half graben’s deep position and geometry of the tectoniclineaments. The Asta is obtained using the tilt angle

References

  • Altınok, S., Karabacak, V.,Yalçıner, C.Ç., Bilgen, A.N., Altunel, E., Kıyak, N.G. 2012. Kütahya fay zonunun Holosen aktivitesi, Türkiye Jeoloji Bülteni, 55, 1.
  • Ansari A. H., Alamdar, K. 2011. A new edge detection method based on the analytic signal of tilt angle (ASTA) for magnetic and gravity anomalies, IJST A2: 81-88, Iranian Journal of Science and Technology.
  • Arısoy, M.Ö., Dikmen, Ü. 2011. Potensoft: MATLAB- based software for potential field data processing, modeling and mapping, Computer and Geoscience, 37, 7, s. 935 – 942.
  • Arpat, E., Bingöl, E.,1969. Ege bölgesi graben sisteminin gelişimi üzerine düşünceler, Maden Tetkik ve Arama Dergisi, 73, 1-9, Ankara.
  • Bhaskara, D., Ramesh, N. 1991. A fortran-77 Computer program for three-Dimensional Analysis of gravity anomalies with variable density contrast, Computer and Geoscience, 17, 5, s. 655-667.
  • Bekler, T., Demirci, A., Özden, S., Kalafat, D. 2011. Simav, Emet fay zonlarındaki optimum kaynak parametrelerinin analizi, 1. Türkiye Deprem Mühendisliği ve Sismoloji Konferansı, ODTÜ, ANKARA.
  • Cooper, G.R.J., Cowan, D.R. 2004. Filtering using variable order vertical derivatives. Computer and Geoscience, 30, 455-459.
  • Cordell, L., Henderson, R.G. 1968. Iterative three- dimensional solution of gravity anomaly data using a digital computer, Geophysics, 33, 596-601.
  • Demirbaş, fi., Uslu A. 1984. Kütahya Simav Gravite Etüdü, Maden Tetkik ve Arama Genel Müdürlüğü Rapor No: 8136, Ankara (unpublished).
  • Doğan, A., Emre, Ö. 2006. Ege graben sisteminin kuzey sınırı: Sındırgı Sincanlı Fay Zonu, 59th. Geological Congress of Turkey, Proceeding Books.
  • Emre, Ö., Duman, T.Y., Duman, fi., Özalp, S. 2012. Türkiye diri fay haritası (yenilenmiş), Maden Tetkik ve Arama Yayınları, Ankara.
  • Gessner, K., Gallardo, L.A., Markwitz, W., Ring, U., Thomson, S.N. 2013. What caused the denudation of the Menderes massif: Rewiev of the crustal evaluation, lithosphere structure, and dynamic topograpy in soutwest Turkey. Gondwana research, 24/1, 243-274
  • Goncalves, W.J. 2006. Inversion gravimetrica 3d de la subcuenca de maturin Üniversidat Simon Bolivar proyekto de grado thesis. Van Hinsbergen, J.J. 2010. A key extensional metamorphic complex rewieved and restored: The Menderes massif of western Turkey, Earth Science Rewievs, 102, 60– 76.
  • Hsu, S.K., Sibuet, J.C., Shyu, C.T., 1996. Depth to magnetic source using generalized analytic signal, Geophysics, 61, 373-386.
  • Kılıç, A.R., Kaya, C., 2010. Simav jeotermal sahasının manyetotellurik yöntemle araştırılması, Yer Elektrik Çalıştayı, Kastamonu.
  • Koralay, O. E., Candan, O., Akal, C., Dora, Ö., Chen, F., Satır, M., Oberhansli, R. 2011. Menderes masifindeki Pan-afrikan ve Triyas yaşlı metagranitoyitlerin jeolojisi ve jeokronolojisi, Batı Anadolu, Türkiye, Maden Tetkik ve Arama Dergisi, 142, 69-121.
  • Miller, H. G., Sing, V. 1994. Potential field tilt - A new concept for location of potential field sources: Journal of Applied Geophysics, 32, 213-217
  • MTA, TÜBİTAK, C.Ü., A.Ü., 2012. 105G145 No’lu Tübitak, Maden Tetkik ve Arama Genel Müdürlüğü, Sivas Cumhuriyet Üniversitesi, Ankara Üniversitesi İşbirliği Projesi, 2012. Kuzeybatı Anadolu Kabuk Yapısının Jeofizik Verilerle Araştırılması Projesi”, 2008- 2012, Ankara (unpublished).
  • Nabighian, M.N. 1972. The analytic signal of two dimensional magnetic bodies with polygonal crossection: it’s properties and use for automated anomaly interpretation, Geophysics, 37, 507-517.
  • Pedersen, L. B. 1989, Retations between horizontal and vertical gradients of potential fields Geophysics, 54, 662-663.
  • Roest, W. R., Verhoef, J., Pilkington, M. 1992. Magnetic Interpretation using the 3-D analytic Signal Geophysics, 1, 116-125, January 1992.
  • Salem, A., Williams, S., Fairhead, D., Ravat, D. V., Smith, R. 2007. Tilt-depth method: A simple depth estimation method using first-order magnetic derivatives: The Leading Edge, December, 1502- 1505.
  • Sarı, C. 2003. Gravite verilerinin tekil değer ayrıştırma yöntemi ile ters çözümü ve Gediz ve Büyük Menderes grabenlerinin tortul kalınlıklarının saptanması, DEÜ Mühendislik Fakültesi Fen ve Mühendislik Dergisi, 5, 1.
  • Seyitoğlu, G. 1997. The Simav Graben: An example of young E-W trending structures in the late cenosoic extensional system of western Turkey. Turkish Journal of Earth Science, 6, 135-141, TÜBİTAK, Turkey.
  • Verdusco, B., Fairhead, J.D., Green, C.M. 2004. New insigth in to magnetic derivatives for structural mapping, Leading Edge, 23 (2), 116-119.
Year 2014, , 119 - 135, 01.06.2014
https://doi.org/10.19111/bmre.81669

Abstract


References

  • Altınok, S., Karabacak, V.,Yalçıner, C.Ç., Bilgen, A.N., Altunel, E., Kıyak, N.G. 2012. Kütahya fay zonunun Holosen aktivitesi, Türkiye Jeoloji Bülteni, 55, 1.
  • Ansari A. H., Alamdar, K. 2011. A new edge detection method based on the analytic signal of tilt angle (ASTA) for magnetic and gravity anomalies, IJST A2: 81-88, Iranian Journal of Science and Technology.
  • Arısoy, M.Ö., Dikmen, Ü. 2011. Potensoft: MATLAB- based software for potential field data processing, modeling and mapping, Computer and Geoscience, 37, 7, s. 935 – 942.
  • Arpat, E., Bingöl, E.,1969. Ege bölgesi graben sisteminin gelişimi üzerine düşünceler, Maden Tetkik ve Arama Dergisi, 73, 1-9, Ankara.
  • Bhaskara, D., Ramesh, N. 1991. A fortran-77 Computer program for three-Dimensional Analysis of gravity anomalies with variable density contrast, Computer and Geoscience, 17, 5, s. 655-667.
  • Bekler, T., Demirci, A., Özden, S., Kalafat, D. 2011. Simav, Emet fay zonlarındaki optimum kaynak parametrelerinin analizi, 1. Türkiye Deprem Mühendisliği ve Sismoloji Konferansı, ODTÜ, ANKARA.
  • Cooper, G.R.J., Cowan, D.R. 2004. Filtering using variable order vertical derivatives. Computer and Geoscience, 30, 455-459.
  • Cordell, L., Henderson, R.G. 1968. Iterative three- dimensional solution of gravity anomaly data using a digital computer, Geophysics, 33, 596-601.
  • Demirbaş, fi., Uslu A. 1984. Kütahya Simav Gravite Etüdü, Maden Tetkik ve Arama Genel Müdürlüğü Rapor No: 8136, Ankara (unpublished).
  • Doğan, A., Emre, Ö. 2006. Ege graben sisteminin kuzey sınırı: Sındırgı Sincanlı Fay Zonu, 59th. Geological Congress of Turkey, Proceeding Books.
  • Emre, Ö., Duman, T.Y., Duman, fi., Özalp, S. 2012. Türkiye diri fay haritası (yenilenmiş), Maden Tetkik ve Arama Yayınları, Ankara.
  • Gessner, K., Gallardo, L.A., Markwitz, W., Ring, U., Thomson, S.N. 2013. What caused the denudation of the Menderes massif: Rewiev of the crustal evaluation, lithosphere structure, and dynamic topograpy in soutwest Turkey. Gondwana research, 24/1, 243-274
  • Goncalves, W.J. 2006. Inversion gravimetrica 3d de la subcuenca de maturin Üniversidat Simon Bolivar proyekto de grado thesis. Van Hinsbergen, J.J. 2010. A key extensional metamorphic complex rewieved and restored: The Menderes massif of western Turkey, Earth Science Rewievs, 102, 60– 76.
  • Hsu, S.K., Sibuet, J.C., Shyu, C.T., 1996. Depth to magnetic source using generalized analytic signal, Geophysics, 61, 373-386.
  • Kılıç, A.R., Kaya, C., 2010. Simav jeotermal sahasının manyetotellurik yöntemle araştırılması, Yer Elektrik Çalıştayı, Kastamonu.
  • Koralay, O. E., Candan, O., Akal, C., Dora, Ö., Chen, F., Satır, M., Oberhansli, R. 2011. Menderes masifindeki Pan-afrikan ve Triyas yaşlı metagranitoyitlerin jeolojisi ve jeokronolojisi, Batı Anadolu, Türkiye, Maden Tetkik ve Arama Dergisi, 142, 69-121.
  • Miller, H. G., Sing, V. 1994. Potential field tilt - A new concept for location of potential field sources: Journal of Applied Geophysics, 32, 213-217
  • MTA, TÜBİTAK, C.Ü., A.Ü., 2012. 105G145 No’lu Tübitak, Maden Tetkik ve Arama Genel Müdürlüğü, Sivas Cumhuriyet Üniversitesi, Ankara Üniversitesi İşbirliği Projesi, 2012. Kuzeybatı Anadolu Kabuk Yapısının Jeofizik Verilerle Araştırılması Projesi”, 2008- 2012, Ankara (unpublished).
  • Nabighian, M.N. 1972. The analytic signal of two dimensional magnetic bodies with polygonal crossection: it’s properties and use for automated anomaly interpretation, Geophysics, 37, 507-517.
  • Pedersen, L. B. 1989, Retations between horizontal and vertical gradients of potential fields Geophysics, 54, 662-663.
  • Roest, W. R., Verhoef, J., Pilkington, M. 1992. Magnetic Interpretation using the 3-D analytic Signal Geophysics, 1, 116-125, January 1992.
  • Salem, A., Williams, S., Fairhead, D., Ravat, D. V., Smith, R. 2007. Tilt-depth method: A simple depth estimation method using first-order magnetic derivatives: The Leading Edge, December, 1502- 1505.
  • Sarı, C. 2003. Gravite verilerinin tekil değer ayrıştırma yöntemi ile ters çözümü ve Gediz ve Büyük Menderes grabenlerinin tortul kalınlıklarının saptanması, DEÜ Mühendislik Fakültesi Fen ve Mühendislik Dergisi, 5, 1.
  • Seyitoğlu, G. 1997. The Simav Graben: An example of young E-W trending structures in the late cenosoic extensional system of western Turkey. Turkish Journal of Earth Science, 6, 135-141, TÜBİTAK, Turkey.
  • Verdusco, B., Fairhead, J.D., Green, C.M. 2004. New insigth in to magnetic derivatives for structural mapping, Leading Edge, 23 (2), 116-119.
There are 25 citations in total.

Details

Primary Language English
Subjects Engineering
Journal Section Articles
Authors

Ceyhan Ertan Toker This is me

Publication Date June 1, 2014
Published in Issue Year 2014

Cite

APA Toker, C. E. (2014). GEOPHYSICAL ANALYSIS AND MODELLING OF THE SİMAV BASIN, WESTERN ANATOLIA. Bulletin of the Mineral Research and Exploration, 148(148), 119-135. https://doi.org/10.19111/bmre.81669
AMA Toker CE. GEOPHYSICAL ANALYSIS AND MODELLING OF THE SİMAV BASIN, WESTERN ANATOLIA. Bull.Min.Res.Exp. June 2014;148(148):119-135. doi:10.19111/bmre.81669
Chicago Toker, Ceyhan Ertan. “GEOPHYSICAL ANALYSIS AND MODELLING OF THE SİMAV BASIN, WESTERN ANATOLIA”. Bulletin of the Mineral Research and Exploration 148, no. 148 (June 2014): 119-35. https://doi.org/10.19111/bmre.81669.
EndNote Toker CE (June 1, 2014) GEOPHYSICAL ANALYSIS AND MODELLING OF THE SİMAV BASIN, WESTERN ANATOLIA. Bulletin of the Mineral Research and Exploration 148 148 119–135.
IEEE C. E. Toker, “GEOPHYSICAL ANALYSIS AND MODELLING OF THE SİMAV BASIN, WESTERN ANATOLIA”, Bull.Min.Res.Exp., vol. 148, no. 148, pp. 119–135, 2014, doi: 10.19111/bmre.81669.
ISNAD Toker, Ceyhan Ertan. “GEOPHYSICAL ANALYSIS AND MODELLING OF THE SİMAV BASIN, WESTERN ANATOLIA”. Bulletin of the Mineral Research and Exploration 148/148 (June 2014), 119-135. https://doi.org/10.19111/bmre.81669.
JAMA Toker CE. GEOPHYSICAL ANALYSIS AND MODELLING OF THE SİMAV BASIN, WESTERN ANATOLIA. Bull.Min.Res.Exp. 2014;148:119–135.
MLA Toker, Ceyhan Ertan. “GEOPHYSICAL ANALYSIS AND MODELLING OF THE SİMAV BASIN, WESTERN ANATOLIA”. Bulletin of the Mineral Research and Exploration, vol. 148, no. 148, 2014, pp. 119-35, doi:10.19111/bmre.81669.
Vancouver Toker CE. GEOPHYSICAL ANALYSIS AND MODELLING OF THE SİMAV BASIN, WESTERN ANATOLIA. Bull.Min.Res.Exp. 2014;148(148):119-35.

Cited By

NAŞA SOKULUMU VE TEKTONİK ANLAMI
Maden Tetkik ve Arama Dergisi
C. Ertan TOKER
https://doi.org/10.19076/mta.346159

THE NAŞA INTRUSION and it’s TECTONIC IMPLICATION
Bulletin Of The Mineral Research and Exploration
C. Ertan TOKER
https://doi.org/10.19111/bulletinofmre.410597

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