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Seismogenic faulting of the sedimentary sequence and laterally variable material properties in the Zagros Mountains (Iran) revealed by the August 2014 Murmuri (E. Dehloran) earthquake sequence

Abstract:

We present source models for the August 2014 Murmuri (Dehloran) earthquake sequence in the Zagros Mountains of Iran. An Mw6.2 mainshock was followed by an aftershock sequence containing five events of Mw ≥ 5.4. Models of P and SH waveforms show that all events had dominantly thrust-faulting mechanisms, and had centroid depths that place them within the thick sedimentary sequence, above the crystalline basement. The combination of our estimated focal mechanisms, relative relocations of the eve...

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Publication status:
Published
Peer review status:
Peer reviewed
Version:
Publisher's version

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Publisher copy:
10.1093/gji/ggv365

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Institution:
University of Oxford
Department:
Oxford, MPLS, Earth Sciences
Role:
Author
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Publisher:
Oxford University Press Publisher's website
Journal:
Geophysical Journal International Journal website
Volume:
203
Issue:
2
Pages:
1436-1459
Publication date:
2015-11-05
DOI:
EISSN:
1365-246X
ISSN:
0956-540X
URN:
uuid:ca2613ab-c4dd-46a8-a18b-e45283147dad
Source identifiers:
593228
Local pid:
pubs:593228

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