Abstract:
The study area located in the north west of Unity State, south central of Muglad Rift Basin. It is bounded approximately by Latitudes 09o17’ and 09o26’ N and Longitudes 29o 5’ and 29o10’ E
A simplified interpretation has been established from integrated well data, lithology logs, porosity logs and resistivity logs data focusing on Tendi formation in the Kaikange area in the Muglad Basin, southern Sudan.
Tendi formation characterized by intercalated between thin sandstone and claystone beds with good porosity in sandstone, the porosity average is more than 28 %. In this study many zones were selected showing good indicator of porosity and saturation.