Textural studies on red sediments of Bhimunipatnam, Andhra Pradesh, east coast of India

• Published in: Journal of the Geological Society of India 2017-07, Vol.90 (1), p.111-117
• Main Authors: Murali Krishna, K. N., Reddy, K. S. N., Ravi Sekhar, Ch, Ganapathi Rao, P., Bangaku Naidu, K.
• Format: Article
• Language: English
• Subjects: Atmospheric precipitations; Carbonates; Chemical precipitation; Clay; Clay minerals; Coastal environments; Color; Colour; Concretions; Dunes; Earth and Environmental Science; Earth Sciences; Energy; Environmental conditions; Garnets; Geology; Grain size; Hydrogeology; Hydroxides; Iron; Minerals; Oxidation; Pebbles; Quaternary; Sand; Sediment; Sedimentary structures; Sediments; Sequencing; Silt; Turbulence; Weathering
• ISSN: 0016-7622; 0974-6889
• DOI: 10.1007/s12594-017-0670-3

The study presents the textural characteristics of late Quaternary red sediments of Bhimunipatnam to understand the process of formation of these sediments. The red sediments are classified into (a) yellow sediments (b) reddish brown sediments (c) brick red sediments and (d) light yellow sediments sequence in the vertical litho section. The yellow sediments, rests on the khondalite basement, comprises of medium grained, moderate to poorly sorted and positively skewed. The rounded pebble beds with trough cross bedding indicate high energy turbulent conditions of deposition. The fining upward sequences indicate sediments were deposited under decreasing energy conditions under fluvial regime.The iron bearing minerals like garnets and pyriboles have undergone chemical weathering under high oxidizing environment resulting in addition of silt and clay to the reddish brown and brick red sediments and concretions were formed by carbonate precipitation. These processes caused changes in the mean grain size and sorting nature of these sediments which are originally aeolian in origin. The light yellow sediments were medium to fine grained, well sorted and similar to modern dune sands in terms of textural parameters. These sediments were deposited under low oxidation environmental conditions and acquired yellow colour due to Fe hydroxides.