The making of Mt Everest: channel flow and low-angle normal faults in the compressional Himalayan orogen

Abstract

Mt Everest (8849 m) spans the Greater Himalayan Sequence metamorphic rocks and the base of the unmetamorphosed Tethyan sedimentary rocks in the Nepal–South Tibet Himalaya. Two north-dipping, low-angle normal faults cut the massif: the upper Qomolangma Detachment placing Ordovician sedimentary rocks above Everest Series greenschist–amphibolite facies rocks; and the lower Lhotse Detachment placing Everest Series schists above sillimanite gneisses, migmatites and leucogranites. The two faults merge northwards into one large ductile shear zone (the South Tibetan Detachment). Pressure–temperature constraints and structural restoration show that the South Tibetan Detachment acted as a passive roof fault during extrusion of the footwall. At least 120 km of southward flow of the footwall rocks occurred during the Miocene, resulting in the exhumation of rocks that were buried to 5.5 kbar (c. 18–22 km depth) below the detachment, juxtaposing them against hanging wall rocks that are essentially unmetamorphosed. The low-angle normal faults were operative during north–south convergence and reflect the exhumation of a locked passive roof fault, unrelated to any crustal extensional processes. U–(Th)–Pb dating of peraluminous leucogranites exposed on Mt Everest (21–20 Ma), Nuptse (c. 19–18 Ma) and along the Rongbuk valley (15.6–15.4 Ma) show that ductile extrusion occurred during the Early Miocene, with brittle faulting at <15.4 Ma during exhumation.