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I. Mechanics of Thrusts and Nappes |
University College, London
Three models of thrust formation have been proposed: sliding opposed by friction, movement by flow in a thin layer, and spreading by more general flow. The field evidence suggests that the shear stresses involved must be low. Experimental and theoretical rock mechanics provide criteria which may be able to distinguish the applicability of the three models, with the constraint of low shear stresses, and the present paper investigates this possibility.