This study examines the Paleoproterozoic history of supracrustal rocks in the western Canadian Shield to better inform the tectonic history of northern Laurentia. Samples for detrital zircon U-Pb geochronology and Hf isotopes were collected from the western Rae Province, Taltson magmatic zone, and the Great Slave Lake shear zone in order to assess depositional ages, provenance and geodynamic significance of the detrital systems. Samples from the western Rae Province were sourced locally and deposited after 2.1 Ga in a broadly extensional regime, based on widespread source terrane ages and few data near the maximum depositional age as well as coeval regional mafic magmatism and absence of coeval metamorphism. By contrast, the Taltson samples were deposited after 2.0 Ga, have a significant 2.2 to 2.0 Ga detrital source of relatively juvenile material, have young zircon that overlap in age with the Taltson and Thelon orogens, and yield a significant fraction of the dates that are close to the maximum depositional age. These Taltson samples were also derived from western Rae Province sources or Buffalo Head and Chinchaga domain sources and are interpreted to have formed in a contractional or collisional regime coeval with Taltson-Thelon orogeny. The 2.2 to 2.0 Ga detritus was likely derived from reworked ca. 2.3 Ga juvenile source. A sample from the Great Slave Lake shear zone was deposited after 2.0 Ga in a contractional/collisional regime and was sourced from Slave Province crust and Taltson-Thelon plutons. Our data support extension along the western Rae Province margin at ca. 2.1 Ga and distinct histories of the Rae and Slave Provinces prior to their collision at ca. 1.95 Ga. Before 2.1 Ga, the Rae Province may have been attached to the Slave, North China, Bastar, Dharwar, or Sinhghbum cratons.