1887
  1. Home
  2. Conferences
  3. Conference Proceedings
  4. 9th Congress of the Balkan Geophysical Society
  5. Conference paper

Abstract

Summary

Konya – Cumra region has several rock formations from different time periods as a result of the location’s geological past. The Bouguer anomaly map shows abnormally high values around Konya Basin where only Cretaceous clastics visible on the surface. The anomaly is studied using spectral analysis and modelled using vertical prisms method in order to achieve a rough underground structure model. The modelling carried assuming a single layer with constant mean depth and density contrast; however, the extra mass calculations carried after modelling process makes other conclusions possible. One of the simplest explanation for the anomaly is an obducted oceanic crust block which may be emplaced during or right after the closing of Thetis Ocean. Another possible explanation is a magmatic intrusion that may have resulted from subduction during closing of Thetis Ocean. Both these theses explain the high Bouguer Anomaly in the Konya – Cumra area, depending on density contrast.

© EAGE Publications BV
Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201702558
2017-11-05
2024-04-19

  • From This Site

    /content/papers/10.3997/2214-4609.201702558
    dcterms_title,dcterms_subject,pub_keyword
    -contentType:Journal -contentType:Contributor -contentType:Concept -contentType:Institution
    10
    5
Loading full text...

Full text loading...

References

  1. Cogley, J. G.
    [1984]. Continental Margins and the Extent and Number of Continents. Reviews of Geophysics22 (2), 101–122.
     [Google Scholar]
  2. Genç, T.
    [1997]. Jeofizikte Modelleme. N.Canıtez içinde, Gravite ve Manyetik Yöntemlerde Modelleme (s. 57–84). İstanbul: Literatür Yayınları.
     [Google Scholar]
  3. Kaya, A. G., & Kılcı, H.
    [2011]. Konya İl Çevre Durum Raporu. Konya: T.C. Çevre ve Şehircilik Bakanlığı Konya Çevre ve Şehircilik İl Müdürlüğü ÇED Hizmetleri Şubesi.
     [Google Scholar]
  4. MTA
    MTA. [2002]. 1/500.000 Ölçekli Jeoloji Haritaları. Maden Tetkik ve Arama Genel Müdürlüğü. Retrieved from: http://www.mta.gov.tr/v2.0/daire-baskanliklari/jed/index.php?id=500bas
     [Google Scholar]
  5. Okay, A., Parlak, O., & Ustaömer, T.
    [2009]. Anadolu Kenet Kuşaklarının Tektonik Ortamı ve Gelişimindeki Problemler ve Olası Çözümleri. 62nd Geological Kurultai of Turkey (s. 445–501). Ankara: MTA.
     [Google Scholar]
  6. Parker, R. L.
    [1972]. The Rapid Calculation of Potential Anomalies. 447–455.
     [Google Scholar]
  7. Rogers, N., Blake, S., & Burton, K.
    [2008]. An introduction to our dynamic planet. Cambridge University Press, 19.
     [Google Scholar]
  8. Talwani, M., & Ewing, M.
    [1960]. Rapid Computation of Gravitational Attaction of Three Dimensional Bodies of Arbitrary Shape. Geophysics, 203–225.
     [Google Scholar]
  9. Öksüm, E., Etiz, A., & Dolmaz, M. N.
    [2005]. Gravite Anomalilerinin Üç Boyutlu (3-B) Modellenmesine Dayanılarak Yapı Derinliğinin Belirlenmesine Bir Yaklaşım. İstanbul Üniversitesi Mühendislik Fakültesi Yerbilimleri Dergisi, 219–227.
     [Google Scholar]
http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201702558
Loading
Gravity Modelling Of Cumra-Konya Region Bouguer Anomalies
Conference Proceedings 2017, 1 (2017); https://doi.org/10.3997/2214-4609.201702558
/content/papers/10.3997/2214-4609.201702558
/content/papers/10.3997/2214-4609.201702558
Loading

Data & Media loading...

Most Cited This Month Most Cited RSS feed

This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error