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Atom Probe Tomography Analysis of Exsolved Mineral Phases
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¿Tectónica de las placas intermitente?

Paul G Silver1, Mark D Behn

  • 1Department of Terrestrial Magnetism, Carnegie Institution of Washington, 5241 Broad Branch Road, NW, Washington, DC 20015, USA.

Science (New York, N.Y.)
|January 5, 2008
PubMed
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Este resumen es generado por máquina.

La subducción puede no ser continua, ya que el cierre de los océanos puede detenerla globalmente. La Tierra La Tierra La Tierra La Tierra La Tierra

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Área de la Ciencia:

  • Geodinámica y tectónica de placas.
  • Ciencias planetarias Ciencias planetarias.
  • Ciencias de la Tierra Ciencias de la Tierra

Sus antecedentes:

  • La subducción continua es una suposición común en las ciencias de la Tierra.
  • Las zonas de subducción pueden terminar debido al cierre de los océanos y al ensamblaje de supercontinentes.
  • El cierre de cuencas de tipo Pacífico podría reducir significativamente la subducción global.

Objetivo del estudio:

  • Para investigar la hipótesis de que la subducción no ha operado continuamente a lo largo de la historia de la Tierra.
  • Explorar las consecuencias de las variaciones del flujo de subducción en la evolución térmica y continental de la Tierra.

Principales métodos:

  • Análisis de la evidencia geológica para el cierre de cuencas tipo Pacífico en el pasado.
  • Evaluación de los mecanismos para la terminación de la subducción y la compensación de inicio.
  • Revisión de los datos que apoyan un mínimo en el flujo de subducción durante el Mesoproterozoico.

Principales resultados:

  • La evidencia sugiere que el cierre de cuencas tipo Pacífico ha ocurrido en el pasado de la Tierra.
  • No hay un mecanismo de compensación directa para la pérdida / ganancia de subducción.
  • Los datos indican un mínimo potencial en el flujo de subducción global en el Mesoproterozoico.

Conclusiones:

  • Se plantea la hipótesis de reducciones dramáticas o cesaciones temporales de la subducción para la historia de la Tierra.
  • Las variaciones en la continuidad de subducción tienen implicaciones significativas para la evolución planetaria.
  • Comprender la historia de la subducción es crucial para comprender el desarrollo térmico y continental de la Tierra.