Tc. Devaraju et Sd. Khanadali, LATERITIC BAUXITE PROFILES OF SOUTH-WESTERN AND SOUTHERN INDIA - CHARACTERISTICS AND TECTONIC SIGNIFICANCE, Current Science, 64(11-12), 1993, pp. 919-921
The lateritic bauxite profiles occur widely distributed as cappings ov
er the high plateaus and hill ranges in the inland areas and coastal t
racts of southern Peninsular India. There is an undoubted genetic conn
ection between the profiles and the underlying bed rocks, which largel
y include the Precambrian charnockite, leptynite, khondalite and Penin
sular Gneisses and the Tertiary Deccan volcanics. The profiles have de
veloped by intense in situ chemical weathering under tropical-subtropi
cal climatic conditions. Available geomorphological and palaeobotanica
l evidence is strongly suggestive of the formation of these profiles m
ostly during the Tertiary period when the landforms had attained tecto
nic stability and the conditions were favourable for lateritization/ba
uxitization.