Crustal structure, restoration and evolution of the Greater Himalaya in Nepal-South Tibet: implications for channel flow and ductile extrusion of the middle crust
Recent suggestions that the Greater Himalayan Sequence (GHS) represents a mid-crustal channel of low viscosity, partially molten Indian plate crust extruding southward between two major ductile shear zones, the Main Central thrust (MCT) below, and the South Tibetan detachment (STD) normal fault abov...
Κύριοι συγγραφείς: | Searle, M, Law, R, Jessup, M |
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Μορφή: | Journal article |
Γλώσσα: | English |
Έκδοση: |
2006
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Παρόμοια τεκμήρια
Παρόμοια τεκμήρια
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Structural evolution and vorticity of flow during extrusion and exhumation of the Greater Himalayan Slab, Mount Everest Massif, Tibet/Nepal: Implications for orogen-scale flow partitioning
ανά: Jessup, M, κ.ά.
Έκδοση: (2006) -
Crustal-lithospheric structure and continental extrusion of Tibet
ανά: Searle, M, κ.ά.
Έκδοση: (2011) -
Channel flow and ductile extrusion of the high Himalayan slab - the Kangchenjunga-Darjeeling profile, Sikkim Himalaya
ανά: Searle, M, κ.ά.
Έκδοση: (2005) -
Mid-crustal deformation of the Annapurna-Dhaulagiri Himalaya, central Nepal: An atypical example of channel flow during the Himalayan orogeny
ανά: Parsons, A, κ.ά.
Έκδοση: (2016) -
Locking of southward extrusion in favour of rapid crustal-scale buckling of the Greater Himalayan sequence, Nar valley, central Nepal
ανά: Godin, L, κ.ά.
Έκδοση: (2006)