Análisis del estrés de transferencia de la secuencia de terremotos deTurquía, Mw7. 8 y Mw 7. 5, 2023
DOI:
https://doi.org/10.62325/10.62325/yachana.v12.n2.2023.891Palabras clave:
Sismo, terremoto, ingeniería sísmicaResumen
Este documento relata los cambios que se han obtenido en los dos grandes terremotos que han azotado a Turquía con diferentes epicentros. El 6 de febrero 2023, se produjo un terremoto de Mw = 7.8 al sur de Turquía, con epicentro cerca de la frontera norte de Siria. Este evento telúrico tuvo un segundo terremoto 9 horas más tarde, por un movimiento de Mw =7.5 alrededor de 90 km al norte. El Mw= 7.8 y las réplicas inscritas se las puede encontrar en la zona de transición de fallas dos falla: Mar Muerto y Oriental de Anatolia. El terremoto con su ubicación preliminar se lo coloca en las cercanías de una triple unión: Placa Arábiga y africana y por último el bloque de Anatolia. Esta última falla adapta el movimiento hacia el oeste de Turquía hacia el Mar Egeo, por otro lado, la falla del Mar Muerto adecúa el movimiento hacia el norte de Arabia en su península con relación a la placa africana. Evento que rompió una brecha sísmica de más de 200 kilómetros de largo y 40 kilómetros de ancho. El objetivo es de contribuir y dar a comprender el papel del estrés de transferencia de la secuencia de terremotos en evolución de Turquía. El uso de instrumentos y conocimientos estadísticos permitieron pronosticar la distribución futura de réplicas y así poner a consideración la posibilidad de terremotos primarios ulteriores; siendo un punto de partida para futuros terremotos de igual o mayor magnitud.
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