We give a reappraisal of the lithostratigraphy of the central Siguiri Basin.
We support this reappraisal with SHRIMP dating of detrital and igneous zircons.
We suggest that the central Siguiri Basin is part of the Tarkwa Group.
These late basin sediments highlight the early architecture of the Siguiri Basin.
This early architecture can be used to improve orogenic gold targeting.