Viscosity of the asthenosphere from glacial isostatic adjustment and subduction dynamics at the northern Cascadia subduction zone, British Columbia, Canada

Late glacial sea level curves located in the Cascadia subduction zone (CSZ) fore arc in southwestern British Columbia show that glacial isostatic adjustment (GIA) was rapid when the Cordilleran Ice Sheet collapsed in the late Pleistocene. GIA modeling with a linear Maxwell rheology indicates that th...

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Veröffentlicht in:	Journal of Geophysical Research. B. Solid Earth 2009-04, Vol.114 (B4), p.n/a
Hauptverfasser:	James, Thomas S., Gowan, Evan J., Wada, Ikuko, Wang, Kelin
Format:	Artikel
Sprache:	eng
Schlagworte:	Earth sciences Earth, ocean, space Exact sciences and technology glacial isostatic adjustment mantle viscosity Marine subduction zone
Online-Zugang:	Volltext
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