Shear-driven upwelling induced by lateral viscosity variations and asthenospheric shear: A mechanism for intraplate volcanism-Reference-Cited by-同舟云学术

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Shear-driven upwelling induced by lateral viscosity variations and asthenospheric shear: A mechanism for intraplate volcanism

Published:2010-02 Issue:3-4 Volume:178 Page:162-175
ISSN:0031-9201
Container-title:Physics of the Earth and Planetary Interiors
language:en
Short-container-title:Physics of the Earth and Planetary Interiors

Author:

Conrad Clinton P.,Wu Benjun,Smith Eugene I.,Bianco Todd A.,Tibbetts Ashley

Publisher

Elsevier BV

Subject

Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics

Reference81 articles.

1. The thermal state of the upper mantle: no role for mantle plumes;Anderson;Geophys. Res. Lett.,2000

2. An analysis of variations in isentropic melt productivity;Asimow;Philos. Trans. R. Soc. Lond. A,1997

3. Non-hotspot volcano chains originating from small-scale sublithospheric convection;Ballmer;Geophys. Res. Lett.,2007

4. A gravity current model of cooling mantle plume heads with temperature-dependent buoyancy and viscosity;Bercovici;J. Geophys. Res.,1996

5. Secondary Hawaiian volcanism formed by flexural arch decompression;Bianco;Geochem. Geophys. Geosys.,2005

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