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- W2044244537 endingPage "1417" @default.
- W2044244537 startingPage "1389" @default.
- W2044244537 abstract "The Protopangaea-Palaeopangaea model for the Precambrian continental crust predicts quasi-integrity reflecting a dominant Lid Tectonics defined by a palaeomagnetic record showing prolonged near-static polar behaviour during very long time intervals (~2.7–2.2, 1.5–1.2, and 0.75–0.6 Ga). Intervening times show polar loops radiating from the geometric centre of the crust explaining the anomalous Precambrian magnetic inclination bias. The crustal lid was a symmetrical crescent-shaped body confined to a single hemisphere on the globe comparable in form to the Phanerozoic supercontinent (Neo)Pangaea. There were two major transitions in the tectonic regime when prolonged near-static motion was succeeded by widespread tectonic-magmatic activity, and each coincided with the major isotopic/geochemical signatures in the Precambrian record. The first comprised a ~90° reconfiguration of crust and mantle at ~2.2 Ga terminating the long 2.7–2.2 Ga static interval; the second was the largest continental break-up event in..." @default.
- W2044244537 created "2016-06-24" @default.
- W2044244537 creator A5036983501 @default.
- W2044244537 date "2014-08-13" @default.
- W2044244537 modified "2023-10-14" @default.
- W2044244537 title "The Precambrian supercontinent Palaeopangaea: two billion years of quasi-integrity and an appraisal of geological evidence" @default.
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