Detrital Zircon Fission-Track Thermochronology of the Present-Day River Drainage System in the Mt. Kailas Area, Western Tibet: Implications for Multiple Cooling Stages of the Gangdese Magmatic Arc
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://link.springer.com/content/pdf/10.1007/s12583-020-1285-y.pdf
Reference74 articles.
1. Bernet, M., 2013. 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. Geosciences, 3(3): 528–542. https://doi.org/10.3390/geosciences3030528
2. Bernet, M., Garver, J. I., 2005. Fission-Track Analysis of Detrital Zircon, Low-Temperature Thermochronology. Techniques, Interpretations, and Applications, 58: 205–237. https://doi.org/10.2138/rmg.2005.58.8
3. Bernet, M., van der Beek, P., Pik, R., et al., 2006. Miocene to Recent Exhumation of the Central Himalaya Determined from Combined Detrital Zircon Fission-Track and U/Pb Analysis of Siwalik Sediments, Western Nepal. Basin Research, 18(4): 393–412. https://doi.org/10.1111/j.1365-2117.2006.00303.x
4. Bernet, M., Zattin, M., Garver, J. I., et al., 2001. Steady-State Exhumation of the European Alps. Geology, 29(1): 3–38. https://doi.org/10.1130/0091-7613(2001)029<0035:sseote>2.0.co;2
5. Brandon, M. T., 1992. Decomposition of Fission-Track Grain-Age Distributions. American Journal of Science, 292(8): 535–564. https://doi.org/10.2475/ajs.292.8.535
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