Dynamics of Subducting Slabs: Numerical Modeling and Constraints from Seismology, Geoid, Topography, Geochemistry, and Petrology
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Elsevier
Reference542 articles.
1. Hydrated subducted crust at 100–250 km depth;Abers;Earth and Planetary Science Letters,2000
2. Seismic low-velocity layer at the top of subducting slabs: Observations, predictions, and systematics;Abers;Physics of the Earth and Planetary Interiors,2005
3. The thermal structure of subduction zones constrained by seismic imaging: Implications for slab dehydration and wedge flow;Abers;Earth and Planetary Science Letters,2006
4. New mantle convection models reconcile conflicting evidence;Albarede;Eos, Transactions of the American Geophysical Union,1999
5. Slab stress and strain rate as constraints on global mantle flow;Alisic;Geophysical Research Letters,2010
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