When Wyoming Became Superior: Oblique Convergence Along the Southern Trans‐Hudson Orogen
Author:
Affiliation:
1. U.S. Geological Survey Denver CO USA
Funder
U.S. Geological Survey
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GL092970
Reference54 articles.
1. The North American Central Plains Conductivity Anomaly
2. Tectonic evolution of the Manitoba-Saskatchewan segment of the Paleoproterozoic Trans-Hudson Orogen, Canada
3. The Pelican Thrust Zone: basal detachment between the Archean Sask Craton and Paleoproterozoic Flin Flon Glennie Complex, western Trans-Hudson Orogen
4. Crustal structure and evolution of the Trans-Hudson orogen: Results from seismic reflection profiling
5. Digital data grids for the magnetic anomaly map of North America
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