Crustal Seismic Discontinuities Under Mexico City Observed With Receiver Functions
Date: 4/26/2019
Time: 06:00 PM
Room: Grand Ballroom
Mexico City is the seat of the Mexican government and the most populated city of the country. It was settled on top of a sedimentary basin which cause amplification to seismic waves of large subduction earthquakes occurring at the Pacific Coast, more than 350 km away, as well as for near intraplate earthquakes, such as the 19 September 2017, Mw7.1, Puebla-Morelos earthquake.
With the purpose of improving our knowledge of the seismic structure of the city and reducing the uncertainty when modeling strong motion in the basin, an ambitious experiment started in May 2017. This experiment consists in installing from 18-22 broadband stations for 3 to 5 days in a site to continuously record; the stations are then relocated to a new site for a similar period, integrating a dense grid of measuring points with ~500 m spacing. Additionally, 18 stations which have been recording continuously since 2010, from the ‘Red Sísmica del Valle de México’(RSVM) are available. We also use data from nine stations of the MesoAmerican Subduction Experiment, a previous array that crossed Mexico City from south to north between 2014 and 2015; and a permanent broadband station of Servicio Sismológico Nacional (SSN, National Seismological Service, Mexico)
In this work, we obtain receiver functions, from both the temporal and permanent RSVM and SSN stations. Despite the small number of teleseisms registered in the temporary array, but given the small distance between stations, it is possible to identify the Ps converted waves from the Mohörovic discontinuity, as well as from other shallower crustal discontinuities. Furthermore, it is possible to differentiate the receiver functions that have gone through shallow low-velocity layers from the ones that have not, being able to identify the presence of the lake sediments. This project has been funded by Secretaría de Ciencia y Tecnología e Innovación (SECITI), project SECITI/073/2016.
Presenting Author: Olivia D. Pita-Sllim
Authors
Olivia D Pita-Sllim oliv.dayanara@gmail.com Universidad Nacional Autónoma de México, Mexico City, , Mexico Presenting Author
Corresponding Author
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Xyoli Perez-Campos xyoli@igeofisica.unam.mx Universidad Nacional Autónoma de México, Mexico City, , Mexico |
Manuel J Aguilar-Velázquez manuel.aguilar.411@gmail.com Universidad Nacional Autónoma de México, Mexico City, , Mexico |
Miguel Rodríguez miguel561a@gmail.com Universidad Nacional Autónoma de México, Mexico City, , Mexico |
Adriana González adrianag@sismologico.unam.mx Universidad Nacional Autónoma de México, Mexico City, , Mexico |
Víctor H Espinosa victore@sismologico.unam.mx Universidad Nacional Autónoma de México, Mexico City, , Mexico |
Delia Bello delia@sismologico.unam.mx Universidad Nacional Autónoma de México, Mexico City, , Mexico |
Luis Quintanar luisq@igeofisica.unam.mx Universidad Nacional Autónoma de México, Mexico City, , Mexico |
Leonardo Ramírez-Guzmán lramirezg@iingen.unam.mx Universidad Nacional Autónoma de México, Mexico City, , Mexico |
Arturo Cárdenas arturo@sismologico.unam.mx Universidad Nacional Autónoma de México, Mexico City, , Mexico |
Jesús Pérez jesus@sismologico.unam.mx Universidad Nacional Autónoma de México, Mexico City, , Mexico |
Iván Rodríguez-Rasilla ivan@sismologico.unam.mx Universidad Nacional Autónoma de México, Mexico City, , Mexico |
Crustal Seismic Discontinuities Under Mexico City Observed With Receiver Functions
Category
Structural Seismology: From Crust to Core