Coseismic Offsets due to Intermediate Depth 16 April 2013 Southeast Iran Earthquake (M-w 7.8)
DSpace at IIT Bombay
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Title |
Coseismic Offsets due to Intermediate Depth 16 April 2013 Southeast Iran Earthquake (M-w 7.8)
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Creator |
KUNDU, B
NANKALI, H MALIK, P YADAV, RK GAHALAUT, VK |
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Subject |
MAKRAN SUBDUCTION ZONE
P-WAVE DEFORMATION MEGATHRUST BENEATH |
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Description |
The 16 April 2013 southeast Iran earthquake (M-w 7.8) is the second major earthquake in the region, including the Makran subduction zone, since 1945. This intraslab earthquake, within the subducting Arabian plate, occurred as a result of normal faulting at an intermediate depth. We report coseismic offsets from the two nearby continuously operating Global Positioning System sites that are located within 300 km of the epicenter. The coseismic offsets are consistent with the slip on the northward steeply dipping fault plane. This earthquake probably occurred in response to the slab- detachment process, and its occurrence has implications for the plate interface coupling of the Makran subduction zone.
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Publisher |
SEISMOLOGICAL SOC AMER
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Date |
2014-12-29T04:32:55Z
2014-12-29T04:32:55Z 2014 |
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Type |
Article
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Identifier |
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 104(3)1562-1566
0037-1106 1943-3573 http://dx.doi.org/10.1785/0120130269 http://dspace.library.iitb.ac.in/jspui/handle/100/17085 |
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Language |
English
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