“…These rivers played a significant role to feed the deltas along the edge of the Indo‐Tethyan Ocean (Biswas, 1999; Mukherjee, 1983). Throughout the Lower Cretaceous epoch, elevated areas and local highs contributed sedimentary deposits to the basins in western India as well as the Indus Basin, extending into present‐day Pakistan (Figure 12; after Aziz et al, 2018; Beaumont et al, 2019, 2023; Bhatt et al, 2016; Biswas, 1999; Bladon et al, 2015; Dolson et al, 2015; Imraz et al, 2013). Most researchers believed that sediments of the WIRBs are mostly sourced from the ADFB and other palaeohighs situated to the north and east of the basinal area (Figure 12; Ahmad & Akhtar, 1990; Akhtar & Aquil, 1984; Biswas, 1987; Beaumont et al, 2019, 2023; Chaudhuri, Das, et al, 2020; Chaudhuri et al, 2023).…”