Neoarchean supracrustal rocks in central Ennadai-Rankin greenstone belt represent ensimatic deposition well-removed from a continental influence. Henik Group...
Three lithotectonic domains outcrop in a transect across east-central Angikuni Lake: I)greenschist facies mafic volcanic and gabbroic rocks; II) upper...
U-Pb ages of detrital zircons from the Paleoproterozoic Hurwitz Group establish depositional age limits for the upper part of the group (Watterson and Tavani...
Henik Group (Neoarchean) supracrustal rocks, including iron-formation marker horizons, were deposited in a deep- water lava plain-slope-basin setting across at...
In the central part of the Ennadai- Rankin belt, Neoarchean iron formation units of the Henik Group have been mapped from the Ducker lake area ca. 35 km north...
Paragneiss near Angikuni Lake, Nunavut contains large, low-CaO garnet porphyroblasts(type I), enveloped by gneissic layering, and post-tectonic, thin garnet...
Sensitive high-resolution ion microprobe (SHRIMP) U-Pb dates on in situ monazite grains areinterpreted to yield an age of 1886 " 6 Ma for the approximately 6...
The dominant U-Pb age of detrital zircons in three stratigraphically enigmatic sandstone units from the central part of the western Churchill Province ranges...