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- W2016453318 abstract "The Altun Shan is a tectonic block to the south of the Tarim basin, North Tibet, bounded to the south by the Altyn Tagh fault. U/Pb crystallisation ages on zircons are 441 ± 9 Ma. 40Ar/39Ar analysis on muscovite yields an age of 383 ± 7 Ma. Both indicate a cooling rate of 7.3 ± 0.6 °C·Ma−1 from 441 to 383 Ma. Further cooling, probably due to exhumation, began at this time and continued at a rate of 0.8 ± 0.3 °C·Ma−1 From three apatite fission-track analyses, cooling rate increased to 8 ± 2 °C·Ma−1 at 10 Ma. L'Altun Shan est un bloc tectonique situé au sud du bassin du Tarim (Nord Tibet) et bordé au sud par la faille de l'Altyn Tagh. L'âge U/Pb sur zircons, de cristallisation du granite AT68 est de 441 ± 9 Ma. L'analyse 40Ar/39Ar sur muscovites donne un âge de 383 ± 7 Ma. Ces datations montrent un taux de refroidissement de 7,3 ± 0,6 °C·Ma−1. Le refroidissement engendré par l'exhumation commence alors avec un taux de 0,8 ± 0,3 °C·Ma−1. Trois analyses des traces de fission sur apatites montrent une augmentation du taux de refroidissement (8 ± 2 °C·Ma−1) vers 10 Ma." @default.
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- W2016453318 date "1999-11-01" @default.
- W2016453318 modified "2023-09-30" @default.
- W2016453318 title "Histoire de l'exhumation de l'Altun Shan: indications sur l'âge de la subduction du bloc du Tarim sous le système de l'Altyn Tagh (Nord Tibet)" @default.
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- W2016453318 doi "https://doi.org/10.1016/s1251-8050(00)88495-5" @default.
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