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  1. Home
  2. Imagen De La Distribución De La Viscosidad Transitoria Después Del Terremoto De Kumamoto De 2016
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  2. Imagen De La Distribución De La Viscosidad Transitoria Después Del Terremoto De Kumamoto De 2016

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Imagen de la distribución de la viscosidad transitoria después del terremoto de Kumamoto de 2016

James D P Moore1, Hang Yu2, Chi-Hsien Tang3

  • 1Earth Observatory of Singapore, Nanyang Technological University, Singapore. earth@jamesdpmoore.com sbarbot@ntu.edu.sg.

Science (New York, N.Y.)
|April 15, 2017

Ver abstracta en PubMed

Resumen
Este resumen es generado por máquina.

Los científicos usaron la secuencia del terremoto de Kumamoto de 2016 para mapear la deformación de la roca y las variaciones de viscosidad en la corteza de Japón. Esta investigación revela zonas de baja viscosidad bajo los volcanes, mejorando nuestra comprensión de los peligros tectónicos.

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Área de la Ciencia:

  • * Geofísica de la Tierra sólida
  • * Tectonofísica
  • * Volcanología

Sus antecedentes:

  • * La deformación de las rocas en respuesta al estrés es fundamental para comprender los riesgos sísmicos y volcánicos.
  • * Las variaciones espaciales de la reología de las rocas (viscosidad) son poco conocidas debido a las dificultades de medición.
  • * Los procesos tectónicos, desde la deriva continental hasta el desencadenamiento de terremotos, están controlados por la deformación de las rocas.

Objetivo del estudio:

  • * Para obtener imágenes directas de deformaciones rocosas localizadas y distribuidas utilizando una perturbación de tensión natural.
  • * Investigar las variaciones espaciales de la reología de las rocas de la corteza y del manto.
  • * Comprender la relación entre la reología de las rocas y la actividad volcánica y sísmica.

Principales métodos:

  • * Utilizó los cambios de estrés causados por la secuencia de terremotos de Kumamoto en 2016.
  • * Aplicación de técnicas geodésicas a los patrones de deformación de imágenes.
  • * Propiedades reológicas inferidas (viscosidad efectiva) de la deformación observada.

Principales resultados:

  • * Se han identificado regiones distintas de baja viscosidad efectiva en la corteza inferior.
  • * Se encontraron zonas de baja viscosidad localizadas debajo de los volcanes Monte Aso y Monte Kuju.
  • * Se han observado variaciones de viscosidad a gran escala en la región del arco posterior japonés.

Conclusiones:

  • * La secuencia de terremotos de Kumamoto de 2016 brindó una oportunidad única para estudiar la reología de las rocas in situ.
  • * La geodesia puede sondear eficazmente la reología de las rocas a través de varias escalas espaciales y temporales.
  • * La comprensión de las variaciones de viscosidad localizadas es clave para evaluar los riesgos volcánicos y sísmicos.