Dergiler / Turkish Journal of Earth Sciences / 2019 / Cilt: 28 - Sayı: 6

Frequency-dependent body-Q and coda-Q in Karlıova Triple Junction and its vicinity, eastern Turkey

Sayfa
902–919
Yayın Tarihi
2022-11-03
DOI
—
🏛️Bu makalenin bibliyografik verileri ve tam metin bağlantısı DergiPark üzerinden sağlanmıştır.
DergiPark Kaydı ↗
✨

Yapay Zeka Hızlı Bakış & Çıkarımlar

AI Insight
⚡ TL;DR(1 Cümlede Hızlı Çıkarım)

The magnitude range was between 2.8 and 6.1 with shallow (

📌 3 Maddede Bu Makale

🎯
Amaç & Hipotez:A dataset obtained from six broadband stations of 111 small- to moderate-sized local events that occurred between 2010and 2018 was analyzed to reveal the frequency-dependent seismic body (body-Q) and coda (coda-Q) wave attenuation characteristicsof three tectonic branches of the Karlıova Triple Junction: the Varto Fault Zone (VFZ), North Anatolian Fault Zone (NAFZ), and EastAnatolian Fault Zone.
📊
Temel Bulgular & Veri:A dataset obtained from six broadband stations of 111 small- to moderate-sized local events that occurred between 2010and 2018 was analyzed to reveal the frequency-dependent seismic body (body-Q) and coda (coda-Q) wave attenuation characteristicsof three tectonic branches of the Karlıova Triple Junction: the Varto Fault Zone (VFZ), North Anatolian Fault Zone (NAFZ), and EastAnatolian Fault Zone.
💡
Sonuç & Katkı:The magnitude range was between 2.8 and 6.1 with shallow (
🔬Tür:Araştırma Makalesi
📍Kapsam:2018 Verileri
⚙️Değişkenler:Alan Parametreleri

Abstract

A dataset obtained from six broadband stations of 111 small- to moderate-sized local events that occurred between 2010and 2018 was analyzed to reveal the frequency-dependent seismic body (body-Q) and coda (coda-Q) wave attenuation characteristicsof three tectonic branches of the Karlıova Triple Junction: the Varto Fault Zone (VFZ), North Anatolian Fault Zone (NAFZ), and EastAnatolian Fault Zone. The magnitude range was between 2.8 and 6.1 with shallow (

🔖

Bu Makaleye Atıf Yap

DEMİRCİ, A. (2022). Frequency-dependent body-Q and coda-Q in Karlıova Triple Junction and its vicinity, eastern Turkey. Turkish Journal of Earth Sciences, Cilt: 28 - Sayı: 6, 902–919. https://ajindex.com/articles/603044

📄 Tam Metin PDF Okuyucu

📄

PDF görüntüleyici hazırlanıyor...

Kaynakça (16)

  1. Abercrombie RE (1997). Near surface attenuation and site effects from comparison of surface and deep borehole recordings. Bulletin of the Seismological Society of America 87: 731-744.
  2. Akıncı A, Eyidogan H (1996). Frequency-dependent attenuation of S and coda waves in Erzincan region (Turkey). Physics of the Earth and Planetary Interiors 97 (1): 109-119.
  3. Akıncı A, Malagnini L, Sabetta F (2010). Characteristics of the strong ground motions from the 6 April 2009 L’Aquila earthquake, Italy. Soil Dynamics and Earthquake Engineering 30: 320-335.
  4. Aki K (1969). Analysis of the seismic coda of local earthquakes as scattered waves. Journal of Geophysical Research 74: 615-31.
  5. Aki K, Chouet B (1975). Origin of coda waves: source, attenuation and scattering effects. Journal of Geophysical Research 80: 3322-3342.
  6. Aki K (1980). Attenuation of shear-waves in the lithosphere for frequencies from 0.05 to 25 Hz. Physics of the Earth and Planetary Interiors 21: 50-60.
  7. Aksoy E, İnceöz M, Koçyigit A (2007). Lake Hazar basin: a negative flower structure on the East Anatolian fault system (EAFS), SE Turkey. Turkish Journal of Earth Sciences 16: 319-338.
  8. Ambraseys NN, Zapotek A (1968). The Varto-üskıran (Anatolia) earthquake of 19 August 1966, summary of field report. Bulletin of the Seismological Society of America 58 (1): 47-102.
  9. Ambraseys NN, Finkel C (1995). The Seismicity of Turkey and Adjacent Areas. A Historical Review: 1500-1800.
  10. İstanbul, Turkey: Muhittin Salih EREN Publications. Armijo R, Meyer B, Hubert A, Barka A (1999) Westward propagation of the North Anatolian fault into the northern Aegean: timing and kinematics. Geology 27: 267-270.
  11. Bianco F, Castellano M, Del Pezzo E, Ibanez M (1999). Attenuation of short-period waves at Mt. Vesuvius, Italy. Geophysical Journal International 138: 67-76.
  12. Bianco F, Del Pezzo E, Castellano M, Ibáñez MJ, Di Luccio F (2002). Separation of intrinsic and scattering seismic attenuation in the southern Apennine zone Italy. Geophysical Journal International 150: 10-22.
  13. Bora N, Biswas R (2017). Quantifying regional body wave attenuation in a seismic prone zone of northeast India. Pure and Applied Geophysics 174: 1953-1963.
  14. Bozkurt E (2001) Neotectonics of Turkey - a synthesis: Geodinamica Acta 14: 3-30.
  15. Büyüksaraç A, Bektaş Ö (2017). Varto Depremi 19 Ağustos 1966.
  16. İstanbul, Turkey: Çantay Publications (in Turkish). Castro RR, Gallipoli MR, Mucciarelli M (2008). Crustal Q in southern Italy determined from regional earthquakes. Tectonophysics