Exhumation and uplift of the Shillong plateau and its influence on the eastern Himalayas: New constraints from apatite and zircon (U‐Th‐[Sm])/He and apatite fission track analyses

The Shillong plateau is the only raised topography in the foreland of the Himalayas. Located on the trajectory of the Indian Summer Monsoon (ISM), the plateau perturbs the regional distribution of precipitation. As such, the Shillong plateau‐eastern Himalaya‐ISM is a unique system to quantify the couplings between climate, tectonics, and erosion. A change in long‐term erosion rates along‐strike of the Bhutan Himalaya was recently attributed to a climatic modulation due to the uplift of the Shillong plateau. To test this interpretation, it is essential to constrain the timing and rate at which the plateau was uplifted and the amount of partitioning of the India‐Asia convergence into the plateau. We used apatite and zircon (U‐Th‐[Sm])/He and apatite fission track analyses to…