Abstract Detrital zircon geochronology has rapidly evolved into a powerful tool for reconstructing the assembly and dispersal processes of supercontinents. Currently, history Gondwanaland remains highly controversial. Here we focus on detrital Gondwana (Carboniferous–Permian Kokaha Diamictite Jurassic–Cretaceous Sapt Koshi Formation) post-Gondwana (Miocene Tamrang sequences Lesser Himalaya in e...