Detrital Zircon Fission-Track Thermochronology of the Present-Day Isère River Drainage System in the Western Alps: No Evidence for Increasing Erosion Rates at 5 Ma
The Isère River system drains parts of the Western Alps in south-eastern France. Zircon fission-track data of the Isère River and its tributaries show a range of apparent cooling ages from about 7 to 150 Ma. Zircons with Jurassic to early Tertiary cooling ages are derived from partially reset or non...
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| Formaat: | Artigo |
| Taal: | Inglês |
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MDPI AG
2013-08-01
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| Reeks: | Geosciences |
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| Online toegang: | http://www.mdpi.com/2076-3263/3/3/528 |
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