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Both petrologic and microstructural/crystal fabric data indicate that isotherms recorded in the schists and gneisses of the Greater Himalayan Slab (GHS) and located in the footwall to the South Tibetan Detachment System (STDS) have undergone extreme telescoping during penetrative flow associated with southward extrusion of the GHS from beneath the Tibetan Plateau. Within the Rongbuk Valley located to the north of Mount Everest we have made vertical sampling traverses working downward from the STDS into the GHS at Hermit’s Gorge, Rongbuk Monastery

himalayan journal of sciences

Telescoping of isotherms beneath the South Tibetan Detachment, Mount Everest Massif: implications for magnitude of internal flow during extrusi on of the Greater Himalayan Slab