Investigation of Salanda Fault Zone, between Yesiloz and Gumuskent (Nevsehir-Turkey) with PSInSAR
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En este estudio, se investigó la sección de la zona de la falla de Salanda entre el pueblode Yesiloz y Gumuskent (Nevsehir, Turquía) mediante métodos geodésicos, y sedeterminó la cantidad de movimiento en esta zona. En este estudio, con este fin utilizamosun radar de apertura sintética interferométrico de dispersión persistente (PSInSAR) paradeterminar el movimiento de la línea de visión (LOS). Estudios anteriores realizados coníndices geológicos y geomorfológicos han demostrado que la zona de la falla de Salandaestá activa. Por primera vez en este estudio, se utilizaron en el análisis PSInSAR 36imágenes de radar de apertura sintética (SAR) adquiridas entre el 8 de enero de 2020 y el29 de noviembre de 2022. Cuando se analizaron los valores anuales de velocidad delárea de estudio en la dirección LOS, se revelaron valores anuales de subsidencia dehasta 7,6 mm y valores anuales de elevación de hasta 7,2 mm. Estos movimientosindican que la falla de es activa y tiene características de falla normal. Sin embargo,también tiene un componente de deslizamiento dextral.
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