Spatial and temporal evolution of tectonometamorphic discontinuities in the central Himalaya: Constraints from P-T paths and geochronology

- A P-T-t path discontinuity was revealed across the Nyalam Discontinuity in south Tibet.
- The regional-scale shear zone (High Himalayan Discontinuity) within the GHC of Nepal was confirmed.
- Ductile shear along the STD was ~ 5-10 Myr earlier than that along the MCT, but was coeval with the HHD at 25-16 Ma.

Recent studies evoke dispute whether the Greater Himalayan Crystalline Complex (GHC) was exhumed during more than one phase. This contribution investigates the timing of ductile shear along the South Tibetan Detachment (STD), Main Central Thrust (MCT), and hidden discontinuities within the GHC of the central Himalaya. New data from the Nyalam transect, southern Tibet, suggest that ductile shear along the STD was active from ~ 27-25 Ma to ~ 17-15 Ma, whereas ductile shear along the MCT was active from ~ 19-16 Ma to ~ 10-8 Ma. Pseudosection modeling results and published metamorphic ages indicate a P-T-t path discontinuity within the GHC and the upper GHC reached higher peak metamorphic temperatures (ΔT 100 °C), similar peak pressures and older metamorphic ages (~ 5-10 Myr), in favor of the presence of the Nyalam Discontinuity. Summarized results from literature suggest that timing of ductile shear along the STD was ~ 5-10 Myr earlier than that along the MCT across the Nepal, Sikkim and Bhutan Himalayas. In addition, the GHC in Nepal can be separated into two portions by a regional-scale (> 800 km) in-sequence ductile shear zone - the High Himalayan Discontinuity. This shear zone was active coevally with the STD during 25-16 Ma, but ~ 5-10 Myr earlier than the MCT. The High Himalayan Discontinuity could possibly extend to the Sikkim Himalayas, but ends in Bhutan. The identified new architecture suggests that both in-sequence and out-of-sequence tectonometamorphic discontinuities are important components that formed the duplexing structure of the GHC in the central and eastern Himalaya, thus calling for more sophisticated numerical simulation than the current models such as the channel flow and critical taper.