Date of Award


Document Type


Degree Name

Doctor of Philosophy (PhD)



First Advisor

W. S. F. Kidd


In Gonto La valley, southern Tibet, a continuous, planar, ∼10°N dipping detachment horizon juxtaposes Tethyan slates over a footwall of leucogranite that intrudes a S-dipping injection complex layer that I regard as a rotated Southern Tibet Detachment System (STDS) horizon. This is deformed & partially cut by the leucogranite which forms a pluton extending throughout Khula Kangri massif. In collaboration, 208Pb-232Th measurements on 12 monazite grains of the leucogranite gave a crystallization age of 12.5 ± 0.4 Ma. Integrated estimates of magnitude, and rate, of detachment displacement suggest that STDS displacement continued after granite crystallisation for 1–3 m.y. Therefore N-S extension in southern Tibet continued into the Late Miocene. A new geologic map of the Khula Kangri and Kanga Punzum-Monlakarchung High Nimalayan ranges is presented using field, satellite & topographic data. These define a fork in the High Himalaya that results in a repetition of the main geological section. The STDS can be traced around both ranges and is a continuous surface. A simple model of post detachment, scissor faulting and block rotation is proposed. In SE Nanga Parbat Haramosh Massif (NPHM), Pakistan, field and microstructural analysis of strain and sense of shear trends indicate that several km of metasedimentary schists and gneisses are Himalayan Main Mantle Thrust (MMT) footwall rocks rotated to vertical due to NW-SE directed shortening. Near the NPHM summit region, several km of non-coaxially sheared granitic orthogneiss show W over E displacement structures. Although deformation mechanisms appear lower temperature than in the MMT footwall rocks, a major “uplift” structure (the Rupal Chichi shear zone - RCSZ) is proposed. To the SW, an E-over W shear zone (the Diamir Shear Zone - DSZ) that coincides with a syn-kinematically intruded granite (the Jalhari Granite) is recognised. In collaboration, 208Pb-232 Th measurements on monazite grains of the Jalhari indicate displacement has continued from ∼9 to Raikot-DSZ, together with the RCSZ define a conjugate pair that is interpreted to mark a pop-up structure, allowing the skywards displacement of NPHM.