The coast of the Southern Mexican states, Guerrero and Oaxaca, between \(-\,102.0{^\circ }\text {E}\) to \(-\,95.5^{\circ }\text {E}\) and \(15.5{^\circ }\text{N}\)–\(18.0^{\circ }\text {N}\) hosts a prominent geologic structure referred to as the Xolapa sliver. Earth Planet Sci Lett 238:64–77, Manea M, Yoshioka S, Manea VC (2017) Subduction of oceanic plate irregularities in South-Central Mexico and the influence on subduction seismicity. 2016) are physical processes that take place in the study area and may affect the behavior of the sliver.

Additionally only the events with percentage of double couple \(\text {DC}\ge 80\%\) are considered (see Additional file 2). Transcurrent motion at the LVC fault can be estimated from slip vectors of subduction thrust earthquakes occurring on the plate interface. The result, referred to as the surface displacement map, shows the relative deformation caused by the earthquake.". The 7.4- magnitude earthquake prompted evacuations in the region, triggered a tsunami warning and damaged thousands of houses. By using this website, you agree to our The age of the oceanic Cocos plate subducting at the Middle America Trench (MAT) increases from about 10 Ma in the west to about 23 Ma (Manea et al. part may be reproduced without the written permission. The earthquake reported in the Oaxaca region occurred at 10:29 local time – with its epicenter located around 12 km southwest of Santa María Zapotitlán. The difference between the results for two catalogs is explained by the inconsistency in local and teleseismic estimations of earthquake source parameters such as strike, dip and rake for the same events. By benefitting from the availability of both Sentinel-1A and Sentinel-1B imagery, scientists are able to quantify the ground movement in both vertical and east-west directions by combing the radar scans obtained as the satellites flew both south to north and north to south. pas de frais. A damaged building is seen after an earthquake in … Thin gray lines are the plate interface isodepth contours (Hayes 2018). For example, a blue-green-red color cycle represents a relative movement towards the radar, while a red-green-blue color cycle means a deformation away from the radar.”, “The fringes can be unwrapped to allow the conversion into meters.

2012) were used in this study. Powerful normal fault earthquakes can take place in deep-ish parts of slabs, says study coauthor Emmanuel Garcia, a tectonics expert at Kyoto University. In this study, \(T_\text{n}\) is calculated through the approximation of the Mexican trench by a small circle. (2013). Global CMT compilation. Nevertheless, our analysis of local and global CMT catalogs with carefully selected subduction thrust events shows that calculated average rates of the sliver motion are fairly different. Privacy Selection criteria are the same as for the local catalog. The Xolapa sliver is, on average, a \(\sim 105\)-km-wide crustal block located along the coast of Guerrero and Oaxaca states of Mexico, and is limited by a \(\sim 650\)-km-long La Venta-Chacalapa fault zone. However, this … https://doi.org/10.1111/j.1525-1314.2006.00632.x, DeMets C (1992) Oblique convergence and deformation along the Kuril and Japan trenches.

Your opinions are important to us. 1) is located along the Pacific coast of Mexico \(\sim 650\)-km long and \(\sim 50\)–80-km wide (Pérez-Gutiérrez et al. The vertical extents of the thrust and strike-slip faults are allowed to differ (McCaffrey 1992). However, the slip vector azimuths of thrust subduction earthquakes tend to approach plate convergence vectors southeastwards along the coast; so, we assume that this may produce the forearc block compression.

The authors declare that they have no competing interests.

The seismogenic zone extends up to 81 km from the trench and is followed by a wide shallow subhorizontal plate interface at the distance between 115 and 270 km from the trench beneath the Guerrero state (e.g., Kostoglodov et al. Influence of subducting plate morphology on tectonics and seismicity, University of California, San Diego, Keppie JD (2004) Terranes of Mexico revisited: a 1.3 billion year odyssey.

(2010)] in the studied section of the Mexican subduction zone. Apart from that, a prior knowledge of the sliver motion initiation is required to quantify the final sliver displacement. The phenomenon of forearc sliver motion has been observed in different subduction zones. Technical report, Research Center for Urban Safety and Security, Kobe University, McCaffrey R (1992) Oblique plate convergence, slip vectors, and forearc deformation. According to the rigid sliver model of McCaffrey (1992), shear forces on the subduction interface and on the crustal faults depend on the slab dip, fault depths and convergence obliquity. 2016; Kostoglodov et al. The rigid block model developed by McCaffrey (1992) is used in this work to quantify the Xolapa sliver motion and corresponding strike-slip displacement on the LVC fault.

Black lines indicate normal to the trench, blue arrows—convergence velocity, orange arrows—average coseismic slip vectors projected to the surface for each region with 95% error ellipses. Weighted mean coseismic slip vector for the events from the local catalog is computed for each region. This geological process is associated with many of the damaging earthquakes on the Pacific coast of Mexico—including the most recent on 23 June. The authors acknowledge financial support from the PAPIIT IG100617 and CONACYT 284212 projects. Credit: Contains modified Copernicus Sentinel data (2020), processed by ESA, CC BY-SA 3.0 IGO. https://doi.org/10.1007/s00024-015-1211-x, Haq SSB, Davis DM (2010) Mechanics of fore-arc slivers: insights from simple analog models. Ryan and Scholl (1989) observe that oblique subduction in the Aleutian arc created a major right-lateral shear zone, the Hawley Ridge shear zone, that has geomorphical and geophysical characteristics similar to the San Andreas fault in California.

https://doi.org/10.1186/s40623-019-1084-9, DOI: https://doi.org/10.1186/s40623-019-1084-9. Model parameters that describe this motion are further analyzed. While there is currently no way to predict when earthquakes will occur, radar imagery from satellites allow for the effects of earthquakes to be observed. Black arrows indicate direction of convergence; black half-arrows show sinistral motion at the LVF. The results of this study showed the Xolapa sliver has a speed of 5–10 mm/year. The result, referred to as the surface displacement map, shows the relative deformation caused by the earthquake.”. Credit: Contains modified Copernicus Sentinel data (2020), processed by ESA, CC BY-SA 3.0 IGO. 2004). https://doi.org/10.1002/2016JB013080, Wang K, Hu Y, Bevis M, Kendrick E, Smalley R, Vargas RB, Lauría E (2007) Crustal motion in the zone of the 1960 Chile earthquake: detangling earthquake-cycle deformation and forearc-sliver translation.

The study of Villegas-Lanza et al. https://doi.org/10.1029/2007GC001721, Wessel P, Smith WHF (1998) New, improved version of Generic Mapping Tools released. The 7.4-magnitude earthquake prompted evacuations in … 2014). The earthquake focal mechanism parameters are used to calculate \(\gamma\) and \(\psi\) by applying axes rotations. The upcoming Sentinel-1C and Sentinel-1D are in the process of being completed, and the design of the next generation of satellites will begin later this year.”. Open Access This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. Long-term GPS observations show trench parallel motion of the sliver southeastwards at the rate of 6–8 mm/year with respect to the NA plate (Kostoglodov et al. According to Hjörleifsdóttir et al.

According to the results obtained from local and Global CMT catalogs for selected subduction thrust earthquakes, the forearc sliver moves southeastwards with respect to the fixed North America plate at the rate of 10 ± 1 mm/year and 5.6 ± 0.8 mm/year, respectively.

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