Estimación de la subsidencia en torno a la traza de la falla de San Ramón Chile, mediante la técnica SBAS DInSAR usando imágenes TerraSAR-X

[EN] Chile is one of the countries with the highest seismicity in the world and is affected by three types of seismogenic sources; interplate, intraplate and superficial or cortical intraplate. In this context, in the eastern sector of the city of Santiago, capital of Chile, the Falla San Ramón (FSR...

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Bibliographic Details
Authors: Lamperein-Polo, Patricio, Vidal-Páez, Paulina, Pérez-Martínez, Waldo
Format: article
Publication Date:2022
Country:España
Institution:Universitat Politècnica de València (UPV)
Repository:RiuNet. Repositorio Institucional de la Universitat Politécnica de Valéncia
Language:Spanish
OAI Identifier:oai:riunet.upv.es:10251/180425
Online Access:https://riunet.upv.es/handle/10251/180425
Access Level:Open access
Keyword:Falla de San Ramón
SBAS
Subsidencia
Interferometría diferencial
San Ramon Fault
Subsidences
Differencial interferometry
Description
Summary:[EN] Chile is one of the countries with the highest seismicity in the world and is affected by three types of seismogenic sources; interplate, intraplate and superficial or cortical intraplate. In this context, in the eastern sector of the city of Santiago, capital of Chile, the Falla San Ramón (FSR) is located. It is a cortical seismogenic source, which threatens its habitants and the various economic activities that are located in that sector, geological hazards such as earthquakes and mass removals. In relation to the above, this study aims to identify and establish the subsidence areas in a longitudinal strip of the Santiago mountain front and its impact on the neighboring communes to the FSR trace during the years 2011 to 2017. To do this, The DInSAR technique was used with the Small Baseline Subset (SBAS) algorithm through a time series of images from the TerraSAR-X (TSX) satellite. The results show subsidence zones, with average displacements ranging from -13.11 mm to +9.89 mm, with an average annual speed rate of -2.19 to +1.65 mm/year.