1. Exhumation history and Early Cretaceous paleogeography of the Newfoundland margin revealed by detrital zircon U–Pb and fission-track studies of syn-rift Hibernia Formation strata. (February 2023) Authors: Johns-Buss, Emily G.; Beranek, Luke P.; Enkelmann, Eva; Jess, Scott; Matthews, William Journal: Marine and petroleum geology Issue: Volume 148(2023) Page Start: Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
2. Late Jurassic flare‐up of the Coast Mountains arc system, NW Canada, and dynamic linkages across the northern Cordilleran orogen. Issue 5 (12th May 2017) Authors: Beranek, Luke P.; McClelland, William C.; van Staal, Cees R.; Israel, Steve; Gordee, Sarah M. Journal: Tectonics Issue: Volume 36:Issue 5(2017) Page Start: 877 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
3. Late Jurassic syn-rift deposition in the Flemish Pass basin, offshore Newfoundland: Evidence for Tithonian magmatism and Appalachian-Variscan sediment sources from quantitative mineral and detrital zircon U–Pb-Hf isotope studies of Mizzen discovery strata. (December 2022) Authors: Beranek, Luke P.; Nissen, Adam; Murphy, Sandra; Grant, David; Goudie, Dylan; Oldham, Lindsay; Johns-Buss, Emily G. Journal: Marine and petroleum geology Issue: Volume 146(2022) Page Start: Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
4. Late Triassic to Jurassic Magmatic and Tectonic Evolution of the Intermontane Terranes in Yukon, Northern Canadian Cordillera: Transition From Arc to Syn‐Collisional Magmatism and Post‐Collisional Lithospheric Delamination. Issue 2 (17th February 2022) Authors: Colpron, Maurice; Sack, Patrick J.; Crowley, James L.; Beranek, Luke P.; Allan, Murray M. Journal: Tectonics Issue: Volume 41:Issue 2(2022) Page Start: n/a Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗