J. Earth Syst. Sci. (2021) 130:60 Ó Indian Academy of Sciences https://doi.org/10.1007/s12040-020-01551-5 (0123456789().,-volV)(0123456789().,-volV) Mineralogy and geochemistry of the sediments in rivers along the east coast of India: Inferences on weathering and provenance 1 1, 1 SHAIK SAI BABU ,VENIGALLA PURNACHANDRA RAO *, NANNAPANENI SATYASREE , 1 2 2 RAVIPATI VENKATA RAMANA ,MEKALA RAM MOHAN and SARIPOOT SAWANT 1Vignan’s Foundation for Science, Technology and Research (VFSTR), Deemed to be Vignan’s University, Vadlamudi, Guntur 522 213, India. 2CSIR-National Geophysical Research Institute, Uppal Road, Hyderabad 500 007, India. *Corresponding author. e-mail:
[email protected] MS received 25 July 2020; revised 19 November 2020; accepted 25 November 2020 The clay fraction of sediments in the lower reaches of 15 rivers along the east coast of India showed high kaolinite followed by illite and smectite for the rivers dominantly draining the Archaean–Precambrian Terrain (APT), high smectite followed by illite and kaolinite for those draining the Deccan Trap Volcanic Terrain (DVT) and, high illite followed by kaolinite, smectite or chlorite for those draining through Mixed-Lithology Terrain (MLT). The CIA (Chemical Index of Alteration) and PIA (Plagioclase Index of Alteration) values, depletion of Ca, K, Na and Sr and enrichment of Al, Fe and Ti, high Rb/Sr and Th/U ratios of sediments relative to the Upper Continental Crust indicate moderate to intense chemical weathering on source rocks. The average composition of clays exhibits slight enrichment of Fe, Mg, Sc, V, Co, Cr and Ni and depletion of Nb, Zr, Hf, Y and Ta relative to the Post-Archaean average Australian Shale.