Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9728
AuthorsPezzo, G.* 
Merryman Boncori, J. P.* 
Atzori, S.* 
Antonioli, A.* 
Salvi, S.* 
TitleDeformation of the western Indian plate boundary: insights from differential and multi-aperture InSAR data inversion of the 2008, Baluchistan (Western Pakistan) seismic sequence
Issue Date2014
Series/Report no./198 (2014)
DOI10.1093/gji/ggu106
URIhttp://hdl.handle.net/2122/9728
KeywordsRadar interferometry
Satellite geodesy
Seismicity and Tectonics
Continental margins: convergent
Earthquake interaction, forecasting and prediction
Earthquake source observation
Subject Classification04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonics 
AbstractIn this study,we use Differential Synthetic Aperture Radar Interferometry (DInSAR) and multiaperture interferometry (MAI) to constrain the sources of the three largest events of the 2008 Baluchistan (western Pakistan) seismic sequence, namely two Mw 6.4 events only 12 hr apart and an Mw 5.7 event that occurred 40 d later. The sequence took place in the Quetta Syntaxis, the most seismically active region of Baluchistan, tectonically located between the colliding Indian Plate and the Afghan Block of the Eurasian Plate. Surface displacements estimated from ascending and descending ENVISAT ASAR acquisitions were used to derive elastic dislocation models for the sources of the two main events. The estimated slip distributions have peak values of 120 and 130 cm on a pair of almost parallel and near-vertical faults striking NW–SE, and of 50 cm and 60 cm on two high-angle faults striking NE–SW. Values up to 50 cm were found for the largest aftershock on an NE–SW fault located between the sources of the main shocks. The MAI measurements, with their high sensitivity to the north–south motion component, are crucial in this area to accurately describe the coseismic displacement field. Our results provide insight into the deformation style of the Quetta Syntaxis, suggesting that right-lateral slip released at shallow depths on large NW fault planes is compatible with left-lateral activation on smaller NE–SW faults.
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