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- W1982552978 abstract "The surface thermal flux in the Ligurian-Provençal basin is accounted for by a three-component model for the continental margins and a cooling model for the oceanic domain. In the continental margins the surface heat-flux data, corrected for the main perturbations, range from 65–70 to 85–90 mW m−; the background heat flowing out from the asthenosphere is 38 mW m−. Heat-flux data from the oceanic domain indicate that the drifting stage should have begun 4–5 Ma earlier and ended 2–3 Ma later than previously inferred, being consistent with recent paleomagnetic results. A decoupling of Corsica from Sardinia during drifting is also validated by the different periods of oceanic accretion which, in the northern sector, seems to be shorter. The rift stage started in the Oligocene and ended about 27 Ma ago between Sardinia and the Gulf of Lion. The rotation of Corsica and Sardinia, which was accompanied by westward crustal accretion, ended about 17 Ma ago. Such a wider time span for drifting involves a more reliable average spreading rate of 2.5 cm a−. An outline of the development of the basin during each evolutionary stage is drawn." @default.
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- W1982552978 date "1996-05-01" @default.
- W1982552978 modified "2023-09-28" @default.
- W1982552978 title "Heat flux and timing of the drifting stage in the Ligurian-Provençal basin (northwestern Mediterranean)" @default.
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- W1982552978 doi "https://doi.org/10.1016/0264-3707(95)00035-6" @default.
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