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- W2010705667 abstract "The subsidence history of Kilohigok Basin (1.9 Ga), N.W.T., Canada reflects the opening and closing of an ocean basin along the present Thelon Tectonic Zone. The basal sedimentary sequence represents a passive‐margin shelf that faced SE toward the orogen. Following passive‐margin subsidence, tectonic loading occurred resulting in rapid subsidence of the outer shelf margin and simultaneous uplift and erosion of the platform interior; a flexural moat formed subparallel to the Thelon Tectonic Zone. The shelf was subsequently drowned and successively buried by deep‐water flysch, shallow‐marine shelf sediments, and fluvial molasse, forming a foreland basin tapered to the NW. Direct structural evidence for the tectonic load is provided by the leading edge of a thin‐skinned thrust‐fold belt exposed in oblique cross‐section within the SE extremity of the basin. Upright folds at high structural levels can be traced downward to recumbent, tight folds and thrusts near the basement/cover contact documenting increasing shear strain with depth. Overall northwest vergence and about 50% shortening is indicated by fold‐thrust geometry and finite stretching lineations, above a brittle/ductile decollement that roots within the Thelon Tectonic Zone." @default.
- W2010705667 created "2016-06-24" @default.
- W2010705667 creator A5013688746 @default.
- W2010705667 creator A5063822572 @default.
- W2010705667 date "1990-10-01" @default.
- W2010705667 modified "2023-10-14" @default.
- W2010705667 title "Early Proterozoic Collisional Orogeny along the Northern Thelon Tectonic Zone, Northwest Territories, Canada: Evidence from the foreland" @default.
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- W2010705667 doi "https://doi.org/10.1029/tc009i005p01015" @default.
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