Journals / 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

Pages
902–919
Publication Date
2019-12-01
DOI
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AI Summary & Key Takeaways

AI Insight
⚡ TL;DR(Too Long; Didn't Read)

The magnitude range was between 2.8 and 6.1 with shallow (

📌 3 Key Takeaways

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Objective & Hypothesis:A dataset obtained from six broadband stations of 111 small- to moderate-sized local events that occurred between 2010 and 2018 was analyzed to reveal the frequency-dependent seismic body (body-Q) and coda (coda-Q) wave attenuation characteristics of three tectonic branches of the Karlıova Triple Junction: the Varto Fault Zone (VFZ), North Anatolian Fault Zone (NAFZ), and East Anatolian Fault Zone.
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Key Findings & Data:A dataset obtained from six broadband stations of 111 small- to moderate-sized local events that occurred between 2010 and 2018 was analyzed to reveal the frequency-dependent seismic body (body-Q) and coda (coda-Q) wave attenuation characteristics of three tectonic branches of the Karlıova Triple Junction: the Varto Fault Zone (VFZ), North Anatolian Fault Zone (NAFZ), and East Anatolian Fault Zone.
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Conclusion & Impact:The magnitude range was between 2.8 and 6.1 with shallow (
🔬Design:Research Article
📍Scope:2010 Verileri
⚙️Variables:Attenuation · coda normalization method · single backscattering model

Abstract

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

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Cite This Article

DEMİRCİ, A. (2019). 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/189375

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