(Q56430576)

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Descent of the ancient Farallon slab drives localized mantle flow below the New Madrid seismic zone

article by A. M. Forte et al published 23 February 2007 in Geophysical Research Letters

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Descent of the ancient Farallon slab drives localized mantle flow below the New Madrid seismic zone (English)

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main subject

New Madrid Seismic Zone

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2

J. X. Mitrovica

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A. M. Forte

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1

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R. Moucha

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N. A. Simmons

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S. P. Grand

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English

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publication date

23 February 2007

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Geophysical Research Letters

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34

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4

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Mesozoic plate-motion history below the northeast Pacific Ocean from seismic images of the subducted Farallon slab

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Seismology: tectonic strain in plate interiors?

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7 January 2021

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Deep-mantle high-viscosity flow and thermochemical structure inferred from seismic and geodynamic data

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Geodynamic evidence for a chemically depleted continental tectosphere

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THE ENIGMA OF THE NEW MADRID EARTHQUAKES OF 1811–1812

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A mechanical model for intraplate earthquakes: application to the new madrid seismic zone

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Cenozoic subsidence and uplift of continents from time-varying dynamic topography

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Tilting of continental interiors by the dynamical effects of subduction

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Analysing the 1811-1812 New Madrid earthquakes with recent instrumentally recorded aftershocks

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The mantle flow field beneath western North America

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7 January 2021

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Space geodetic evidence for rapid strain rates in the New Madrid seismic zone of central USA.

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7 January 2021

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Seismology: Tectonic strain in plate interiors? (Reply)

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7 January 2021

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252126489

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(Q56430576)

Descent of the ancient Farallon slab drives localized mantle flow below the New Madrid seismic zone

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