Abstract

Seismic Reprocessing of the vintage data has brought out finer depositional elements present in the Kalol Formation. Utilization of spectrally decomposed bands, Seismic Pre/Post Stack Inversion, RMS Amplitudes and various other tools for unraveling the Eocene depositional system in the Cambay Basin basin in India, aided in detailed mapping of various depositional elements and subtle facies variations within them. Through mapping and sequential slicing of the Eocene sequence a full depositional cycle of Kalol formation is interpreted which helped in identifying subtle stratigraphic traps.