•Use three different 3D MT inversion codes for data from Krafla and Hengill in Iceland.•Comparison of resistivity and derived properties highlight structural coincidence.•Strong agreement of larger structures in all models, small structures vary more.•More variation in models in Krafla, nosier data affecting the inversion process.•Structural similarities add confidence and aid appraisal in terms of geology.
Geothermics – Elsevier
Published: Sep 1, 2015
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