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• W2155656263 abstract "Palaeomagnetic measurements, in the Late Triassic-Liasic Zarzaïtine formations of the La Reculée area, showed the existence of superimposed and juxtaposed magnetizations. The separation of the juxtaposed magnetizations yielded Late Triassic-Liasic magnetization directions of normal and reversed polarities. The new corresponding palaeomagnetic pole agrees well with a Pangea A configuration. It confirms, from Autunian to Lias, a latitudinal displacement of stable Africa towards the north, with important anti-clockwise rotation contrary to Laurussia which did not undergo significant rotation. This transition of Pangea from A2 to A ended before the Late Triassic. It corresponds to dextral movements in the Hercyno-Appalachian collision area, and perhaps to part of the northwards drift of microcontinents of Gondwanian origin located north of the Arabian promontory." @default.
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• W2155656263 date "1995-02-01" @default.
• W2155656263 modified "2023-10-03" @default.
• W2155656263 title "A new Late Triassic-Liasic Palaeomagnetic pole from superimposed and juxtaposed magnetizations in the Saharan craton" @default.
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• W2155656263 doi "https://doi.org/10.1111/j.1365-246x.1995.tb01830.x" @default.
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