Fig. 5From: Cenozoic sedimentary records of climate-tectonic coupling in the Western HimalayaSimplified stratigraphy of the western Himalayan foreland basin derived from the work of Jain et al. (2009), showing the general coarsening up-section and the appearance of a variety of higher grade metamorphic minerals that might be associated with the unroofing of the Greater and Inner Lesser HimalayaBack to article page