PNGE 450 EXAM 1 GR Log Flashcards
Introduction
Gamma Ray log measures the natural radioactivity of the formations.
GR is a passive measurement and no energy is provided by the logging tool.
The radioactivity comes from 3 element groups of Uranium, Thorium, and Potassium.
GR is measured in 2 common ways of natural (total natural radioactivity) and
spectral (identifying the contribution of each 3 source elements of U, Th, K).
The GR log can be run in combination with practically any tool available.
Application
Correlation
Indicating the lithology
Identifying of clay minerals
Evaluating shale content (volume) of the formation
Applicable both in open and cased holes.
Compatible with any type of fluid
Origin of Natural GR
Sedimentary rocks tend to emit Gamma rays.
Natural GR originates from 3 element groups of
Uranium (
238U), Thorium (232Th), and Potassium (40K)
Summary
GR log measures the natural radioactivity of formation. It can be total or spectral.
GR log is used for identifying the lithology, clay mineral and evaluating the shale volume.
GR log is used for well to well (open/cased hole) and core to log correlation.
GR log requires borehole effect correction.
GR log is affected by logging speed and time constant. An optimized combination should
be used.