Titlebook: Subduction; Insights from Physic Alexander I. Shemenda Book 1994 Springer Science+Business Media Dordrecht 1994 geodynamics.lithosphere.mod

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0924-6096 of the modeling method (including similarity criteria, anda novel applied experimental technique), results from modelexperiments, theoretical analysis of results on the basis of continuummechanics, and their geodynamic interpretation. Subduction is modeledin general as well as applied to particular

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Jumps of Subduction Zones, Subduction Reversal, and Closing of Back Arc Basins,ung lithosphere, an increase in subduction rate, subduction of different asperities (seamounts, ridges) and plateaux. The most intensive compression occurs during subduction of the continental margin, that is during collision of the subduction zone with a continent. High compressive stresses can pro

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Continental Subduction,n the collision zones beneath either continental or oceanic lithosphere, is defined by the presence of a thick continental crust in the latter case. High buoyancy of the crust prevents it from being pushed or dragged down deep into the mantle. The general picture of the continental lithosphere subdu

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Jumps of Subduction Zones, Subduction Reversal, and Closing of Back Arc Basins, ridges and the jumps of continental rifts.1991]). With jumps of subduction zones are related such processes as reorganization of the plate boundaries, evolution of the inner trench slopes, reversal subduction.1979;.1984], as well as closing of back arc basins. This chapter is devoted to these problems.