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- W1887841294 abstract "Paleomagnetic studies of Paleozoic sedimentary and plutonic rocks demonstrate that the Yucatan Block did not lie between the North and South American plates in the Pangean assembly during the Permian. In the Middle Permian, the Yucatan Block lay in an inverted orientation on the western margin of Pangea at 6–10°S, probably forming part of the NW coast of South America. Subsequently the block rotated in a series of counterclockwise motions as the North and South American plates separated. By 230 Ma, Yucatan had rotated ∼47° counterclockwise and moved slightly northward, to the equator. Counterclockwise rotation continued through the Jurassic: ∼41°..." @default.
- W1887841294 created "2016-06-24" @default.
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- W1887841294 date "2005-01-01" @default.
- W1887841294 modified "2023-09-24" @default.
- W1887841294 title "Pangean reconstruction of the Yucatan Block: Its Permian, Triassic, and Jurassic geologic and tectonic history" @default.
- W1887841294 doi "https://doi.org/10.1130/0-8137-2393-0.457" @default.
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