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Synconvergent ductile flow in variable-strength continental crust; numerical models with application to the western Grenville Orogen
(American Geophysical Union, Washington, DC, 2007-10)
No abstract available.
Evolution of orogenic wedges and continental plateaux: insights from crustal thermal-mechanical models overlying subducting mantle lithosphere
(2003-04)
The links between an early phase of orogenesis, when orogens are commonly wedge shaped, and a later phase, with a plateau geometry, are investigated using coupled thermal-mechanical models with uniform velocity subduction ...