Inhaltsbereich
Publications
(Co) Author: Tao, M.
(since 2001) [ All ]
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(2006): Climatic versus tectonic control on river incision at the margin of NE Tibet: 10Be exposure dating of river terraces at the mountain front of the Qilian Shan.. Journal of Geophysical Research, 111, F03012.
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(2004): Implications of the fault scaling law for the growth of topography: mountain ranges in the broken foreland of north-east Tibet. Terra Nova, 16, 3, 157-162.
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(2004): Late Pleistocene/Holocene slip rate of the Zhangye thrust (Qilian Shan, China) and implications for the active growth of the northeastern Tibetan Plateau. Tectonics, 23, No. 6, TC6006.
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(2003): Combined IRSL-OSL single aliquot regeneration (SAR) equivalent dose (De) estimates from source proximal Chinese loess. Quaternary Science Reviews, 22, 10-13, 975-983.| EDOC: 3608 |
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(2002): 21Ne versus 10Be and 26Al exposure ages of fluvial terraces: the influence of crustal Ne in quartz. Earth and Planetary Science Letters, 201, 575-591.| EDOC: 3239 |
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(2002): Low slip rates and long-term preservation of geomorphic features in Central Asia. Nature, 417, 6887, 428-432.
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(2004): Surface exposure dating of landforms covered by loess.. Scientific Report 2004, Paul Scherrer Institute.| EDOC: 7006 |
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(2003): High preservation potential of geomorphic surfaces in the arid foreland of NE Tibet revealed by exposure dating.. Scientific Report 2003, Vol. 1, Paul Scherrer Institue.| EDOC: 6996 |
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(2002): 21Ne versus 10Be surface exposure ages of quartzite: a comparison. Abstracts of the 12th annual V. M. Goldschmidt conference, 12th Annual V. M. Goldschmidt Conference (Davos, Switzerland, 2002), A326.| EDOC: 6477 |
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(2001): 21Ne versus 10Be surface exposure ages of quartzite: A comparison. 79. Jahrestagung der Deutschen Mineralogischen Gesellschaft (DMG) (Potsdam 2001).| EDOC: 2807 |
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(2001): Slip rates of active thrusts in the Qilian Shan (China) based on 21 Ne and 10Ne surface exposure ages of Late Pleistocene alluvial fans and luminescence dating of Holocene loess deposits. 16. Himalaya-Karakorum-Tibet Workshop.| EDOC: 2812 |