Subduction and eduction of continental crust: major mechanisms .
Geophysical data from orogenic belts in continental collision zones show that collision results in a greatly thickened crust. In the Alps, a maximum Moho depth of.
Quantifying Crustal Thickness in Continental Collisional Belts NCBI
1 Aug 2017 . In the South Qinling Belt, crustal thickening began at ~240 Ma and ... in the partial melting/differentiation mechanisms that collisional belts and.Live Chat