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• W2941686647 abstract "The Phanerozoic history of North America, when viewed from the perspective of Pangea, can be divided into three broad phases with gradational time boundaries, as described in the following paragraphs. During the first phase, which lasted from the late Precambrian to the Pennsylvanian, Pangea was under construction and the North American craton was marked by various, persistent, sedimentary basins—the Michigan, Hudsons Bay, Appalachian, Black Warrior, Arkoma, Tobosa, Illinois, and Williston. The western continental margin was either a divergent (passive) margin, facing the paleo-Pacific Ocean (Panthalassa) or a backarc basin bordering that ocean, while the eastern margin, beginning in the Middle Ordovician, underwent convergent and collisional tectonism, during the various phases of the Appalachian orogen. Phase two, which included the final assembly of Pangea, extended through the Pennsylvanian and Permian, and continued into the Triassic. Most of the cratonic basins became inactive as new stresses were imposed on the continent related to Pangean assembly. The greater Appalachian foreland basin developed adjacent to the Appalachian orogen. The Sverdrup basin formed as a successor basin to the Franklin orogen in the Canadian Arctic. The Slide Mountain and Havallah back-arc basins extended from the Yukon to western Nevada, and the Maritime basins of eastern Canada formed in complex rift-transform settings. The southwestern margin of the continent was affected by oblique-slip displacement between North America and Gondwana (including portions of what are now Mexico and the southwestern United States), with the development of an orogenic highland called the Ancestral Rockies. A host of new basins were formed throughout the region of Southwestern North America affected by the Ancestral Rocky Mountains orogen, an event with unclear relations to the Ouachita-Marathon orogen. Phase three, commencing in the Late Triassic or Early Jurassic, corresponds to the Pangea breakup phase, during which North America drifted northwestwards (relative to a hot-spot reference frame). The eastern continental margin became the modern extensional Atlantic margin, while the western margin underwent accretionary tectonism leading to the assembly of the Cordilleran orogen. Various rift-related basins of eastern North America extended from the Bisbee trough of Arizona to Southeastern Canada. Complex trench, forearc, and backarc basins developed across the Cordillera and the largest North American basin, formed in response to the Sevier orogen, became the site of the Western Interior Seaway. Late Cenozoic basins in the western Cordillera formed in response to widespread transform processes." @default.
• W2941686647 created "2019-05-03" @default.
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• W2941686647 date "2019-01-01" @default.
• W2941686647 modified "2023-10-09" @default.
• W2941686647 title "The Phanerozoic Tectonic and Sedimentary Evolution of North America" @default.
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• W2941686647 doi "https://doi.org/10.1016/b978-0-444-63895-3.00001-2" @default.
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