Magnetic interpretation along the Sudbury Structure Lithoprobe Transect

Magnetic modelling of the Sudbury Structure (SS) has been undertaken using the geometrical and lithological framework provided by high‐resolution seismic reflection data. This initial constraint was required because of the complex magnetic properties exhibited by rock units of the SS. Locally remanent magnetisation (NRM) dominates over induced magnetisation, and the orientation and amplitude of the NRM vector varies both between and within …