Portable gamma apparatus for core analysis and method therefor

An apparatus and method for a wellsite gamma-ray analysis of core samples is implemented. A wheeled carriage supporting a gamma-ray detector stably straddles a core sample, which may be encased in a core barrel. A bracket attached to the carriage may hold a radionuclide source of gamma radiation positioned distally from the detector, thereby forming a space therebetween for passage of the core. The density of the core may be determined by counting the gamma flux attenuated by the core; by traversing the carriage along a length of the core, the density may be determined as a function of position, and disrupted core or partial recovery detected thereby. Additionally, the natural gamma emission of the core may be observed by traversing the apparatus along the core without the radionuclide source.