Postglacial rebound at the northern Cascadia subduction zone
By T. James, John J. Clague, Kelin Wang, I. Hutchinson. 2000
145 citations recorded by the source corpus.
Subfields: Atmospheric Science, Geophysics
View Paper: https://www.semanticscholar.org/paper/cdef3584c15c25ea78c6d800c3ae5a6231ed4699
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In Geophysics
Citations in the corpus
- The thermal structure of subduction zone back arcs (2004, background): “…zones comes from independent observations of the Earth’s surface response to transient crustal loads, for example, postglacial rebound [e.g., James et al., 2000; Ivins and James, 1999], postseismic relaxation [e.g., Wang, 2006, and references therein], and lacustrine loading/unloading…”
- Rheology of the Lower Crust and Upper Mantle: Evidence from Rock Mechanics, Geodesy, and Field Observations (2008, background): “Modeling of shoreline tilts of proglacial lakes and rapid sealevel fall in southwestern British Columbia and Puget Sound following the retreat of the Cordilleran ice sheet suggests upper-mantle viscosities of 5–50 × 1018 Pa s ( James et al. 2000).”