C. Beaumont et al., Himalayan tectonics explained by extrusion of a low-viscosity crustal channel coupled to focused surface denudation, NATURE, 414(6865), 2001, pp. 738-742
Recent interpretations of Himalayan-Tibetan tectonics have proposed that ch
annel flow in the middle to lower crust can explain outward growth of the T
ibetan plateau(1-3), and that ductile extrusion of high-grade metamorphic r
ocks between coeval normal- and thrust-sense shear zones can explain exhuma
tion of the Greater Himalayan sequence(4-7). Here we use coupled thermal-me
chanical numerical models to show that these two processes-channel flow and
ductile extrusion-may be dynamically linked through the effects of surface
denudation focused at the edge of a plateau that is underlain by low-visco
sity material. Our models provide an internally self-consistent explanation
for many observed features of the Himalayan-Tibetan system(8-10).