Abstract

The area of study lies in the Nardipur Low between Kalol and Limbodra Fields towards west and east, respectively (Fig.1).In this area, K-IX sand is the main producer (Eocene age) and K-V is of marginal interest. K-IX sand was deposited in deltaic environment and is seen as channel feature. It is also characterized by marshy -swampy environment marked by coal, shale, sand and silt. An attempt has been made to understand the reservoir facies distribution over the field through seismic inversion study of the 3D seismic data in the area (Fig.2).