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- W2062479968 abstract "The Pangean supercontinent extended and broke apart in the early Jurassic, but an understanding of how and why this event took place when it did has remained elusive. An analysis of the angular velocities governing the global plate circulation during this period reveals that the final closure of the Paleo-Tethys Ocean between Eurasia and Cimmeria and the early opening of the Atlantic Ocean between North America and South America/Africa were governed by symmetric motions sharing a common rotation axis. This symmetry is remarkable and is consistent with a subduction-driven mechanism in the disaggregation of Pangea. A basic hypothesis is that the Eurasia-Cimmeria collision disrupted the clockwise spin of Pangea during the Triassic. Pangea rifted because tensional stresses were redistributed within Pangea following the collision. Rifting was localized across zones of pre-existing thick-skinned weakness within Pangea (late Paleozoic suture zones) which were optimally-oriented parallel to the north Tethyan subduction system." @default.
- W2062479968 created "2016-06-24" @default.
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- W2062479968 date "2014-01-01" @default.
- W2062479968 modified "2023-09-23" @default.
- W2062479968 title "Is the Eurasia-Cimmeria Collision Linked to Pangea Breakup?" @default.
- W2062479968 doi "https://doi.org/10.3997/2214-4609.20141070" @default.
- W2062479968 hasPublicationYear "2014" @default.
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