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Deep conductivity structure in Abitibi, Canada, using long dipole magnetotelluric measurements
Author(s) -
Tournerie Benoit,
Chouteau Michel
Publication year - 1998
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/98gl51690
Subject(s) - magnetotellurics , geology , anisotropy , electrical resistivity and conductivity , seismology , tectonics , geophysics , crust , shearing (physics) , archean , petrology , paleontology , geotechnical engineering , physics , quantum mechanics
Magnetotelluric data recorded in the period range 10²–2.10 4 s using 100 km telluric dipoles in western Quebec, Canada, yield impedance estimates free from galvanic distortion and static shift. Analysis of the apparent resistivity, phase and magnetic transfer function data favors a regional 1D anisotropic model for the subsurface resistivity structure in the Abitibi Subprovince; lower resistivity direction of the anisotropy is EW, parallel to the main fault system. Joint 1D inversion of both principal impedances indicates a conductivity anisotropy in the upper and middle crust and in the upper mantle. It might originate for all depths from the same tectonic mechanism, mainly a NS shortening followed by an EW dextral shearing in the Archean.