Abstract
In the Ogilvie Mountains of west-central Yukon, intrusive breccias and volcanic rocks are aligned along faults that were active during evolution of the Cordilleran miogeocline. Character of the magmatic rocks provide clues to changing lower crust or upper mantle conditions beneath the western margin of ancestral North America.
The unusually long (Middle Proterozoic to Jurassic) sedimentary record was influenced by episodes of crustal stretching. Extensional events are indicated by proximal clastic sequences deposited in half-grabens during extensional faulting. Igneous rocks associated with each stretching event have been dated: hematitic megabreccia (1270 Ma), bimodal tholeiitic volcanic rocks (750 Ma), Cambro-Ordovician alkalic basalt, and mid-Cretaceous alkalic granites (90 Ma).
Although crystalline basement rocks are not exposed in the northern fold and thrust belt, the combination of inferences from the sedimentary record, ancient structures, and igneous chemistry imply recurring zones of weakness and periodic mantle disturbance beneath the ancient continental margin.
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Roots, C.F., Thompson, R.I. (1992). Long-lived basement weak zones and their role in extensional magmatism in the Ogilvie Mountains, Yukon Territory. In: Bartholomew, M.J., Hyndman, D.W., Mogk, D.W., Mason, R. (eds) Basement Tectonics 8. Proceedings of the International Conferences on Basement Tectonics, vol 2. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-1614-5_24
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