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Interpreting gravity measurements (view source)
Revision as of 15:57, 14 March 2016
, 15:57, 14 March 2016no edit summary
==Depth-to-basement determination==
==Depth-to-basement determination==
Gravity is not as good at depth-to-basement or depth-to-density anomaly estimations as other geophysical methods. Though possible to do, it is often difficult to determine the appropriate depth to geologic source unless other constraints exist.
Gravity is not as good at depth-to-basement or depth-to-density anomaly estimations as other [[geophysical methods]]. Though possible to do, it is often difficult to determine the appropriate depth to geologic source unless other constraints exist.
==Positions of geologic bodies==
==Positions of geologic bodies==