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Dynamic Pore-scale Reservoir-condition Imaging of Reaction in Carbonates Using Synchrotron Fast Tomography
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Las réplicas impulsadas por una fuente de CO2 de alta presión en profundidad.

Stephen A Miller1, Cristiano Collettini, Lauro Chiaraluce

  • 1Institute of Geophysics, Swiss Federal Institute of Technology (ETH), 8093 Zürich, Switzerland. steve.miller@erdw.ethz.ch

Nature
|February 20, 2004
PubMed
Resumen
Este resumen es generado por máquina.

Una secuencia de terremotos de 1997 en Italia fue impulsada por un pulso de presión de fluido de dióxido de carbono (CO2) profundo. Este pulso, liberado durante la sacudida principal, desencadenó miles de réplicas, desafiando los modelos tradicionales de terremotos.

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Área de la Ciencia:

  • La geofísica es la geofísica.
  • Sismología Sismología Sismología.
  • La tectónica es la tectónica.

Sus antecedentes:

  • La secuencia de terremotos de 1997 en el norte de Italia, que incluyó dos temblores principales (M5.7, M6) y miles de réplicas, presentó un rompecabezas sismológico.
  • Los modelos tradicionales de transferencia de tensión elástica no pudieron explicar adecuadamente la secuencia de falla normal observada, especialmente la sismicidad persistente de las paredes colgantes.

Objetivo del estudio:

  • Para investigar un mecanismo alternativo que impulsa la secuencia del terremoto de 1997 en el norte de Italia.
  • Para explorar el papel de los pulsos de presión de fluidos en la generación de réplicas de terremotos.

Principales métodos:

  • Análisis de las ubicaciones precisas del hipocentro de las réplicas.
  • Modelado de difusión no lineal para rastrear la propagación de la presión del fluido.
  • Comparación de las amplitudes de pulso de presión del fluido con los cambios de tensión de los modelos elásticos.

Principales resultados:

  • Se encontró una fuerte correlación entre un frente de fluido de alta presión y los hipocentros de réplicas durante dos semanas.
  • El pulso de presión del fluido identificado (10-20 MPa) excedió significativamente los cambios de tensión típicos (0.1-0.2 MPa) de los modelos elásticos.
  • El pulso de presión del fluido se originó a partir de la liberación coseísmica de dióxido de carbono (CO2) profundo y de alta presión.

Conclusiones:

  • La secuencia de terremotos de 1997 probablemente fue impulsada por un pulso de presión de fluido de CO2 profundo liberado.
  • La liberación cosísmica de fluidos atrapados y de alta presión puede generar réplicas en zonas dañadas.
  • Este mecanismo vincula los terremotos, las réplicas, la desgasificación de la corteza y el manto, y el flujo de fluidos a gran escala.