Barrow-Dampier Sub-basin - Australia - 2007
The West Panaeus survey is located in the highly prolific Barrow-Dampier Sub-Basin
The main objective of the survey is to improve the understanding of the stratigraphic framework of the M. australis reservoir in both a regional and local sense.
This data covers the Lewis Trough which is a thick Jurassic depocentre containing large volumes of mature, upper Jurassic Dingo Claystone Formation source rocks and is the SW extension of the Madeleine Trend down towards Barrow Island.
3D seismic data to better understand structural complexity of survey area.