Basaltic andesites of Precambrian age are reported end described for t
he first time from Garo Hills, Meghalabra, These volcanics occur as xe
noliths within Proterozoic granitoids, Petromineralogical and petroche
mical characters of the volcanics revealed them to be basaltic andesit
e, The basaltic andesite are observed both as porphyritic and aphyric
types.