9d) further indicates that the main locus of the afterslip was downdip from the co-seismic rupture (Figs9a andb). The rapid change in magnitude and direction of the plate convergence at the trench reflects the nearby location of the RiveraNorth America pole (red circle in inset map). Supporting Information Fig. This patient may have damage to which of the following?, Injury to cervical vertebra C3-C4 is particularly problematic because _____. 9a) and seismically derived solutions referenced above is encouraging and suggests that our co-seismic slip solution is an adequate basis for the time-dependent modelling that is described in the remainder of this section. 14a), at the southeastern limit of the 1995 rupture zone (Fig. Global Positioning System (GPS) measurements in Jalisco began in the mid-1990s as part of an effort to study the regional subduction earthquake cycle and associated seismic hazards (DeMets etal. For comparison, our 1995 co-seismic slip solution gives an average slip of 1.8m over an area of 13,200km2. We use two types of time-dependent modelling to estimate possible solutions for the interseismic, co-seismic and post-seismic processes that dominate deformation in our study area. More generally, large earthquakes along the Mexican segment of the MAT tend to produce relatively few aftershocks (Singh etal. 20). It can develop in both men and women, particularly in people who smoke, drink excessive amounts of alcohol, take steroid medication, or have a family history of hip fractures. Lin etal. Discuss below determining the postseismic motion is romantic and immature, he stated after Hitler became chancellor Germany! Courboulex etal. 2007). We also estimate the long-term velocities of all the GPS sites fully corrected for the co-seismic and post-seismic effects of the 1995 and 2003 earthquakes. The along-strike variations are particularly well recovered, which indicates that the slip during the 2003 earthquake was strongly concentrated offshore from the southern Colima Graben (Fig. Westward-directed postseismic seafloor displacements may be due flow via low-temperature, plastic creep within the lower half of a Pacific lithosphere weakened by plate bending. A creeping fault, the Hayward fault will rupture they found that 74 percent of the expected incheshad. The afterslip solutions for both earthquakes suggest that most afterslip coincided with the rupture areas or occurred farther downdip and had cumulative moments similar to or larger than the co-seismic moments. Including the June 1932M8 earthquakes, whose rupture areas are known only approximately (Fig. 1). We first subtracted the combined viscoelastic effects of both earthquakes for each of the six assumed mantle Maxwell times from all of the daily GPS position time-series. The fits of the time-dependent model with m = 15yr are good overall (Fig. 2013; Graham etal. The 2.540yr range of Maxwell times we tested is comparable to the 150yr range of Maxwell times used by Suito & Freymueller (2009) to model 30yr of post-seismic deformation in Alaska and also include the 815yr mantle relaxation time limits that Johnson & Tebo (2018) identified by modelling 50 yr of vertical post-seismic deformation in Nankai with a linear Maxwell viscoelastic mantle and afterslip model. The large misfit F values of our solutions (>13) are symptomatic of an undervaluation of the data uncertainties. At the continuous site COLI, which is directly onshore from the 2003 rupture, rapid post-seismic deformation ceased by mid-2003 and the site resumed its pre-1995 northeast-directed motion by 2005 (Figs3, 6 and7). None of our solutions satisfactorily fits all the GPS data. (2002) from their modelling of continuous measurements at site COLI. 2004). Our geodetically derived co-seismic moment, 1.84 1020 Nm (Mw = 7.4), is close to seismologic estimates of Mo = 2.0 1020 Nm (Ekstrm etal. (2001) from their modelling of the first few years of post-seismic data, and with the results from Marquez-Azua etal. The October 9, 1995 ColimaJalisco earthquake, the first along the JCSZ to be geodetically recorded and modelled (Melbourne etal. Panels (c) and (d) respectively show the horizontal and vertical site motions that are predicted by the co-seismic and afterslip solutions from panels (a) and (b) at sites active during the earthquake. Both features of our 1995 afterslip model (i.e. 20). (iii) Resolution of the 2003 earthquake co-seismic slip based on the 35 stations that operated between 1993 and 2005.5 and with data after 2003 (Supporting Information Fig. It is movement following an earthquake that releases the build up of tectonic stress. Best-fitting GPS site velocities from the time-dependent inversion of GPS position time-series that were corrected using a mantle Maxwell time of 15yr (Section5.6 and Supporting Information Table S10). White, yellow and red stars are the epicentres from Yagi etal. We then inverted the noisy synthetic velocities to find the best-fitting interseismic locking solution. (c) Continuous site farther inland. 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