Abstract

This paper presents a new way of flattening the seismic in 3D using a new space/time framework. The parameterization of the seismic data is based on the interpreted faults and main stratigraphic events, and a stratigraphic column is used to grant its geological consistency. The result is a new flattened space where all the horizons are flattened and where any data can be mapped for visualization. Interpretation can be performed in this flattened space, and the result can be mapped back to the regular geological space.