Item talk:Q239423
From geokb
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"name": "Alternative rupture-scaling relationships for subduction interface and other offshore environments",
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"abstract": "Alternative fault-rupture-scaling relationships are developed for Mw 7.1\u2013\n9.5 subduction interface earthquakes using a new database of consistently derived finitefault\nrupture models from teleseismic inversion. Scaling relationships are derived for\nrupture area, rupture length, rupture width, maximum slip, and average slip. These relationships\napply width saturation for large-magnitude interface earthquakes (approximately\nMw >8:6) for which the physical characteristics of subduction zones limit the\ndepth extent of seismogenic rupture, and consequently, the down-dip limit of strong\nground motion generation. On average, the down-dip rupture width for interface earthquakes\nsaturates near 200 km (196 km on average). Accordingly, the reinterpretation of\nrupture-area scaling for subduction interface earthquakes through the use of a bilinear\nscaling model suggests that rupture asperity area is less well correlated with magnitude\nfor earthquakes Mw >8:6. Consequently, the size of great-magnitude earthquakes appears\nto be more strongly controlled by the average slip across asperities.\nThe sensitivity of the interface scaling relationships is evaluated against geographic\nregion (or subduction zone) and average dip along the rupture interface to\nassess the need for correction factors. Although regional perturbations in fault-rupture\nscaling could be identified, statistical significance analyses suggest there is little\nrationale for implementing regional correction factors based on the limited number\nof interface rupture models available for each region.\nFault-rupture-scaling relationships are also developed for intraslab (within the\nsubducting slab), extensional outer-rise and offshore strike-slip environments. For\nthese environments, the rupture width and area scaling properties yield smaller dimensions\nthan interface ruptures for the corresponding magnitude. However, average and\nmaximum slip metrics yield larger values than interface events. These observations\nreflect both the narrower fault widths and higher stress drops in these faulting environments.\nAlthough expressing significantly different rupture-scaling properties from\nearthquakes in subduction environments, the characteristics of offshore strike-slip\nearthquake ruptures compare similarly to commonly used rupture-scaling relationships\nfor onshore strike-slip earthquakes.",
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