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- W2273281607 abstract "The Phanerozoic history in Nebraska and adjacent regions contains many patterns of structure and stratigraphy that can be directly related to the history of the Precambrian basement rocks of the area. A process is proposed that explains the southward growth of North America during the period 1.8–1.6 Ga. A series of families of accretionary events during the Proterozoic emplaced sutures that remained as fundamental basement weak zones. These zones were rejuvenated in response to a variety of continental stress events that occurred during the Phanerozoic. By combining the knowledge of basement history with the history of rejuvenation during the Phanerozoic,..." @default.
- W2273281607 created "2016-06-24" @default.
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- W2273281607 date "2007-01-01" @default.
- W2273281607 modified "2023-10-16" @default.
- W2273281607 title "Precambrian accretionary history and Phanerozoic structures—A unified explanation for the tectonic architecture of the Nebraska region, USA" @default.
- W2273281607 doi "https://doi.org/10.1130/2007.1200(15)" @default.
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