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FRICTIONAL - VISCOUS FLOW IN MYLONITE WITH VARIED BIMINERALICCOMPOSITION AND ITS EFFECT ON LITHOSPHERIC STRENGTH (1999)
A theoretical, composite flow law is presented for mylonite containing interconnected layers of a weak mineral undergoing power law creep and porphyroclasts of a stronger mineral undergoing fracture and frictional sliding.
Reference:
Tectonophysics 303 (1999) 175-191
Tectonophysics 303 (1999) 175-191
Organization:
Institut fur Geowissenschaften, Universitat Giessen, D-35390 Giessen, Germany
Institut fur Geowissenschaften, Universitat Giessen, D-35390 Giessen, Germany
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