Abstract
Detailed geochronological and petrographic studies were carried out in and around Bhawanipatna and Deobhog (Odhisa, India), which are located at the western boundary of the Eastern Ghats Granulite Belt (EGB) adjacent to Bastar Craton. It was believed that up to ?500 Ma EGB was contiguous with the East Antarctica. This study is not only important in terms of establishing geological evolution of this particular area but also significant for better understanding of the Precambrian transcontinental correlation with Proto-India.