The Eastern Highlands shear zone (EHSZ) is located on Cape Breton Island where it separates rocks of the Bras-d'Or and Aspy terranes within Ganderia in the...
Rocks exposed near suture zones can record the timing and style of orogenic accretion events. However, in long-lived accretionary orogens, subsequent...
The Bathurst Fault is a NNW-trending crustal-scale structure that transects through the eastern Slave craton and left-laterally displaces the Thelon tectonic...
On Cape Breton Island, Nova Scotia, the Eastern Highlands Shear Zone bisects the Ganderia composite terrane, separating the Aspy and Bras D'Or terranes. The...
The Eastern Highlands shear zone (EHSZ), in the Cape Breton Island portion of Appalachian Orogen, records two ductile deformation events (D1 and D2) from Early...
Single-grain 40Ar/39Ar dates are reported for detrital white mica from low-grade meta-arkose samples from the Gondwana Formation in the Darjeeling-Sikkim...
Jurassic to Paleogene post-accretionary structures in the northern Canadian Cordillera generally lack absolute timing constraints and their kinematics are only...
The South Mountain Batholith (SMB) is a composite peraluminous intrusion in southwestern Nova Scotia and the largest granitoid body in the Appalachian Orogen....
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