Rocks exposed near suture zones can record the timing and style of orogenic accretion events. However, in long-lived accretionary orogens, subsequent...
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...
The Bathurst Fault is a NNW-trending crustal-scale structure that transects through the eastern Slave craton and left-laterally displaces the Thelon tectonic...
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...
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...
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...
In this research activity, we will attempt to determine the timing and direction of motion for faults, major breaks in the Earth's crust, that formed during...
Jurassic to Paleogene post-accretionary structures in the northern Canadian Cordillera generally lack absolute timing constraints and their kinematics are only...
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