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- W2232557934 abstract "ABSTRACT In the Canadian Arctic Archipelago strata of the Sverdrup Basin rest with pronounced angular unconformity on the Franklinian geosyncline which is composed of a miogeosynclinal and a eugeosynclinal belt. Until recently the oldest strata of the Sverdrup Basin were believed to be Middle Pennsylvanian in age, New fossil collections indicate that in northern Axel Heiberg and Ellesmere Islands the basal unit of the Sverdrup Basin is Late Mississippian (Visean) in age. Mid-Paleozoic orogeny of the Franklinian eugeoyncline took place between Early or Middle Devonian and Late Mississippian times and probably reached its climax in the Late Devonian. Deformation of the miogeosyncline occurred somewhat later, between Late Devonian and Middle Pennsylvanian times, perhaps in the latest Devonian or Early Mississippian. The relations of these movements to contemporaneous orogenies in the Arctic are discussed." @default.
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- W2232557934 date "1962-01-01" @default.
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- W2232557934 title "Mississippian Rocks and the Mid-Palaeozoic Earth-Movements in the Canadian Arctic Archipelago" @default.
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