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The oldest continental foreland basin sediments containing metamorphic detritus eroded from the Himalaya orogeny therefore seem to be at least 15–20 Myr younger than previously believed, and models based on the older age must be re-evaluated.

The Balakot Formation, located in the Hazara–Kashmir Syntaxis of Northern Pakistan, is a continental foreland basin sedimentary sequence that contains detritus eroded from the India–Eurasia suture zone and the metamorphic rocks of the Himalaya8-km-thick fossil-free clastic red bed succession, within which are intercalated four discrete grey fossiliferous marl bands (Fig. Nummulites and assilines biostratigraphy of the marl bands has constrained the succession to 55–50 Myr (latest Palaeocene to Mid Eocene).