Item talk:Q236568
From geokb
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"name": "Ball-and-socket tectonic rotation during the 2013 Mw7.7 Balochistan earthquake",
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"abstract": "The September 2013 Mw7.7 Balochistan earthquake ruptured a \u223c200-km-long segment of the curved Hoshab fault in southern Pakistan with 10\u00b10.2 m of peak sinistral and \u223c1.7\u00b10.8 m of dip slip. This rupture is unusual because the fault dips 60\u00b115\u00b0 towards the focus of a small circle centered in northwest Pakistan, and, despite a 30\u00b0 increase in obliquity along strike, the ratios of strike and dip slip remain relatively uniform. Surface displacements and geodetic and teleseismic source inversions quantify a bilateral rupture that propagated rapidly at shallow depths from a transtensional jog near the northern end of the rupture. Static friction prior to rupture was unusually weak (\u03bc<0.05), and friction may have approached zero during dynamic rupture. Here we show that the inward-dipping Hoshab fault defines the northern rim of a structural unit in southeast Makran that rotates \u2013 akin to a 2-D ball-and-socket joint \u2013 counter-clockwise in response to India's penetration into the Eurasian plate. This rotation accounts for complexity in the Chaman fault system and, in principle, reduces seismic potential near Karachi; nonetheless, these findings highlight deficiencies in strong ground motion equations and tectonic models that invoke Anderson\u2013Byerlee faulting predictions.",
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