We propose a hybrid inversion analysis (hia) technique aimed at incorporating earthquakes from different seismogenic sources in one single inversion scheme. The application of this technique provides estimations of the source, path, and site effects at 23 strong-motion stations in El Salvador, Central America. The strong-motion dataset comprises 404 triaxial accelerograms corresponding to 63 subduction and upper-crustal earthquakes with M S magnitudes between 3.0 and 7.8. Application of the hia technique reveals: (1) good matching of the estimated source spectra with those derived from the ω 2 point source model; (2) rapid and low attenuation patterns characterizing the upper-crustal volcanic belt and subduction zone, respectively; and (3) soil transfer functions characterized by amplification ratios larger than those derived from spectral ratio techniques by a factor of two. Reference- site-dependent techniques yield similar soil transfer functions at all stations, whereas the horizontal-to-vertical spectral ratio technique yields similar results at sites characterized by clearly predominant peaks.
Research Article| July 01, 2003 Earthquake Disasters of 13 January and 13 February 2001, El Salvador Walter Salazar; Walter Salazar Search for other works by this author on: GSW Google Scholar Kazuoh Seo Kazuoh Seo Tokyo Institute of Technology Interdisciplinary Graduate School of Science and Engineering Department of Built Environment 4259 Nagatsuta, Midori-ku Yokohama 226-8502 Japan seo@enveng.titech.ac.jp (K.S.) Search for other works by this author on: GSW Google Scholar Seismological Research Letters (2003) 74 (4): 420–439. https://doi.org/10.1785/gssrl.74.4.420 Article history first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Walter Salazar, Kazuoh Seo; Earthquake Disasters of 13 January and 13 February 2001, El Salvador. Seismological Research Letters 2003;; 74 (4): 420–439. doi: https://doi.org/10.1785/gssrl.74.4.420 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietySeismological Research Letters Search Advanced Search El Salvador is a small country in Central America (Figure 1). It has a savanna climate, with daytime temperatures consistently between 25°–30°C. The rainy season extends from May to October, while November to April is generally very dry. Rainfall is about 1,800 mm per year. These weather conditions are favorable for producing sugar and coffee. The population is about 6.0 million with a high concentration in the capital city, San Salvador, where 1.8 million persons are living now. The earthquakes of 13 January and 13 February 2001 demonstrated the high vulnerability in El Salvador and strongly affected people... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
This book chapter explains the methodology to determine the shear wave velocity VS profile employing microtremors array data at Port of Spain, Trinidad, and its implication in the seismic amplification and liquefaction hazard in the city. We divide this study into five sections; firstly, we introduce a description of the spectral autocorrelation method and the genetic algorithm schemes to retrieve the Vs and thickness of soil layers. Secondly, we validate the soil profiles via inspection of the ellipticity pattern at such sites; we also compared the observed horizontal-to-vertical spectral ratios (H/V) with the synthetic ones derived by the Diffuse Field Approach and 1D theoretical SH wave amplification functions. Thirdly, we compute the shear wave velocity in the first 30 m obtained from our genetic inversion and compared with the ones estimated by the empirical formulas based on geomorphological conditions. Fourthly, we present a preliminary liquefaction hazard map based on the level of H/V microtremor ratios and the fundamental period of vibration. Finally, we conclude with further recommendations for planning purposes in the city of Port of Spain.
This chapter aims to provide a methodology to test the probability distributions of earthquakes in terms of the interoccurrence times (ITs), namely, the time between consecutive earthquakes of a specific magnitude. First, we compile a new earthquake catalog for the El Salvador subduction zone within moment magnitude M 5.0–8.12 comprising historical and instrumental data for 1609–2019. Secondly, we explain the fundamentals of the Weibull and Poisson distributions and verify the IT probability fits when considering the clustered catalog. We find that the Weibull distribution fits all ITs, while the Poisson distribution fails to explain the natural seismicity patterns for small magnitude bins. Besides, we test the assumption that the declustering process leads to a Poisson probability distribution when removing foreshocks and aftershocks in the earthquake catalog. Finally, the classical Gutenberg–Richter relationship and conditional magnitude probabilities are calculated as an essential input in any seismic hazard assessment.
A probabilistic seismic hazard analysis has been performed to compute probabilistic seismic hazard maps for the eastern Caribbean region (10° N-19° N, 59° W-64° W), which includes in the north the Leeward Islands (from Anguilla to Dominica) and in the south the Windward Islands (from Martinique to Grenada), Barbados, Trinidad, and Tobago. The analysis has been conducted using a standard logic-tree approach that allowed systematically taking into account the model-based (i.e., epistemic) uncertainty and its influence on the computed ground motion param- eters. Hazard computations have been performed using a grid of sites with a space resolution of 0.025 degrees covering the territory of the considered islands. Two different computation methodologies have been adopted: the standard Cornell-McGuire approach (Cornell, 1968; McGuire, 1976) based on the definition of appropriate seismogenic zones (SZ), and the zone-free approach developed by Woo (1996), which overcomes the ambiguities related with the definition of seis- mic sources. The interplay and complexities between shallow crustal, intraplate, and interface subduction seismicity of the Caribbean region have been thoroughly investigated. By merging all available databases, a comprehensive and updated earthquake catalog for the region has been compiled. Also, a thorough investigation has been undertaken to identify the most suitable ground motion prediction equa- tions to be used in the analyses. Uniform hazard spectra have been calculated for the horizontal component of ground motion (rock and level site conditions), 4 return periods (RP) (95-, 475-, 975-, and 2475-yr), and 22 spectral accelerations (SA) with structural periods ranging from 0 to 3 s. SAs at 0.2 and 1.0 s for 2475-yr RP have been calculated to allow the definition of seismic hazard in the region of study according to the International Building Code (IBC, International Code Council (ICC), 2009).
La Universidad Centroamericana "José Simeón Cañas" busca aportar con este artículo información técnica en las áreas sismológicas y de ingeniería sísmica para entender mejor los sismos principales ocurridos en El Salvador, en el período de enero y febrero del 2001. Específicamente se presentan y estudian los mismos del 13 de enero y del 13 y 17 febrero del 2001, pues son los que mayor impacto han tenido en toda la serie de eventos de estos dos meses. Así, se explican brevemente conceptos basicos de sismología, necesarios para elaborar aspectos en apartados posteriores; se realiza una reseña de la sismicidad y tectónica de El Salvador y se presentan los parámetros de origen de los sismos estidiados. Posteriormente se presentan los resultados obtenidos en la red de acelerógrafos de la UCA y un análisis breve de los resgistros obtenidos durante estos tres eventos. Finalmente, se hace una lista, a manera de conclusión, de algunos puntos que pueden ser beneficiosos para desarrollar la mitigación del riesgo sísmico.
ECA Estudios Centroamericanos, Vol. 56, No. 627-628, 2001: 11-27.