Large areas of bedrock in Canada, such as in the interior plateau of British Columbia, are covered by a thick glacial overburden. Lateral variations in overburden thickness can create spurious anomalies in gravity data. These anomalies can be of a size and amplitude similar to those associated with mineral bodies and can be mistaken for them. A methodology is introduced that corrects gravity data for changes in overburden thickness through the use of a bedrock topography map created by integrating information from a helicopter transient electromagnetic survey with geological survey data, well water data, and gravel pit locations. The approach is tested for a 68 km × 38 km area in the prospective Nechako interior plateau of British Columbia, Canada. The methodology extends the traditional Bouguer corrections by taking into account the gravitational contribution of the overburden. Results show that the capability of an airborne survey to detect a change in overburden thickness depends primarily on survey line spacing and to a lesser extent on the level of random noise in the gravity data. The bedrock topography correction has the capability of removing the gravitational attraction of overburden for the purpose of revealing, through interpretation, geological structures in the gravity data that originate from the bedrock and are otherwise concealed.
Correcting airborne gravity data for overburden thickness: a case study from the Nechako interior plateau, British Columbia1
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Raymond M. Caron, Claire Samson, Martin Bates, Michel Chouteau; Correcting airborne gravity data for overburden thickness: a case study from the Nechako interior plateau, British Columbia. Canadian Journal of Earth Sciences 2018;; 56 (5): 483–492. doi: https://doi.org/10.1139/cjes-2017-0209
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