“…Owing to their lower mobility in a variety of environments and lesser residence times in seawater (Cox, Lowe, & Cullers, 1995;Taylor & McLennan, 1985), the trace elements and rare earth elements (REEs) are useful in determining the provenance and tectonic settings. Certain immobile trace elements (e.g., V, La, Th, Zr, Hf, Sc, Co, Ni, Cr, and REEs) are used to identify the most likely provenance of a clastic sedimentary rock (Asiedu, Agoe, Amponsah, Nude, & Anani, 2019;Bhatia, 1985;Bhatia & Crook, 1986;Chen et al, 2019;Cullers, 1995;Cullers & Berendsen, 1998;Cullers & Podkovyrov, 2002;Garver & Scott, 1995;Khan, Sarma, Somasekhar, Ramanaiah, & Ramakrishna Reddy, 2019;Ma et al, 2019;Madhavaraju et al, 2020,b;McLennan, 1989;Nagarajan et al, 2014Nagarajan et al, , 2015Nagarajan et al, , 2019Nagarajan, Armstrong-Altrin, et al, 2017;Nagarajan, Roy, et al, 2017).…”