Distinguishing Faults from Flooding Surfaces on Spectral Gamma-Ray Logs

Uranium (Nuclear Minerals) / Exploration, Mining, Marketing, & Acquisitions

Date posted: 02/28/10

A. Ruffell, J. M. McKinley, and R. Evans AAPG Bulletin, v. 88, no. 9 (September 2004), pp. 1239-1254 Elevated gamma-ray emission from discrete beds in sedimentary deposits may conventionally be interpreted as representing flooding surfaces or transgressive beds. Potassium (K), uranium (U), or (less commonly) thorium (Th) concentrations in outcrop or borehole successions cause such elevated gamma-ray emission and may be linked to the presence of specific mineral hosts. Furthermore, specific Th/K and Th/U ratios occur at correlated stratigraphic surfaces and form part of a pattern that reflects a sequence stratigraphic hierarchy. Spectral gamma-ray logs from uncored boreholes or weathered cliffsides and acquired without full petrographic descriptions can intersect low-angle faults such as thrusts. Our study demonstrates that bedding-parallel faults can be mistaken for flooding surfaces.We document the spectral gamma-ray response through a range of visually obvious & cryptic faults.