The Huronian Supergroup is a Proterozoic assemblage of geologic groups of the Superior craton of the Canadian ShieldinOntario and Quebec. It extends from west of the city of Sault Ste. Marie in the west to the Ontario-Quebec border to the east and is part of the Southern Geologic Province.[1][2]
The Huronian Supergroup consists of four groups. All of the rocks are low grade metamorphic sedimentary rocksorigneous rocks.
The four geologic groups that make up the Huronian are the Elliot Lake Group, Hough Lake Group, Quirke Lake Group, and the Cobalt Group (from oldest to youngest). Major glacial periods, Huronian glaciation, occurred at the beginning of the Hough Lake, Quirke Lake and Cobalt.[3]
The bulk of the Huronian Group consists of mostly metamorphosed sandstones and mudstones. Since there are no index fossils, the sedimentary rocks cannot be dated using fossils, like they can in Phanerozoic rocks. However, the base contains volcanic rocks that have been dated at about 2.480 billion years ago (Gya). The top of the Huronian and cross cutting all of the units within are the Nipissing sills which date to 2.2185 Gya. The age at which the Huronian sediments were deposited is between 2.480 Gya and 2.219 Gya.
