Tectonic evolution of the Superior Boundary Zone from coincident seismic reflection and magnetotelluric profiles
Author:
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
http://www.agu.org/journals/tc/v018/i003/1999TC900002/1999TC900002.pdf
Reference56 articles.
1. Ansdell , K. U-Pb constraints on the timing and provenance of fluvial sedimentary rocks in the Flin Flon and Athapapuskow Basins, Flin Flon Domain, Trans-Hudson Orogen Radiogenic Age and Isotopic Studies: Report 7 49 57 Geol. Surv. Of Canada Ottawa 1993
2. U-Pb geochronology and tectonic development of the southern flank of the Kisseynew Domain, Trans-Hudson Orogen, Canada;Ansdell;Precambrian Res.,1995
3. Kisseynew metasedimentary gneiss belt, Trans-Hudson orogen (Canada): Back-arc origin and collisional inversion;Ansdell;Geology,1995
4. A geodynamic framework for interpreting crustal-scale seismic reflectivity patterns in compressional orogens;Beaumont;Geophys. J. Int.,1994
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