The cosmogenic 10Be exposure histories of in situ bedrock surfaces from the Tibetan Plateau indicate low erosion rates of <30 mm/ka in southern and central Tibet during the last interglacial–glacial cycle that contrast strongly with unusually rapid erosion rates (60–2000 mm/ka) for Kunlun in northern Tibet during the Holocene, comparable with published values from the Himalaya. By comparing apatite fission-track ages with cosmogenic data, erosion rates in southern Tibet appear to be decelerating since the Miocene, whereas in the Kunlun, erosion rates have accelerated over the same timescale. Such secular changes suggest that the southern and central regions of the plateau had formed their present flat relief by the Pleistocene. Unusually hi...
Terrestrial cosmogenic nuclide (TCN) exposure dating has become the most dominant technique for cons...
Fluvial incision, regarded as one of the fundamental geomorphic processes, drives the evolution of m...
Global data suggest that erosion rates variously scale with steepness or climate forcing (precipitat...
The cosmogenic 10Be exposure histories of in situ bedrock surfaces from the Tibetan Plateau indicate...
The central Songpan–Ganzi belt, located on the eastern margin of the Tibetan Plateau, has a similar ...
Concentrations of in-situ-produced cosmogenic nuclides 10Be and 26Al in quartz were meas-ured by acc...
This paper builds a database of apatite fission track (AFT) ages and thermal-modeling results coveri...
Concentrations of in-situ-produced cosmogenic nuclides Be-10 and Al-26 in quartz were measured by ac...
International audienceThis contribution provides new constraints on the timing of Tibetan glacial re...
Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/94784/1/tect2305.pd
Quantifying long-term erosion rates across the Tibetan Plateau and its bordering mountains is of cri...
New detrital low-temperature thermochronometry provides estimates of long-term erosion rates and the...
The 5-km-high Tibetan plateau is an outstanding topographic feature on the earth today. Its areal ex...
Fluvial incision, regarded as one of the fundamental geomorphic processes, drives the evolution of m...
The Tibetan Plateau holds an ample record of past glaciations, and there is an extensive set of glac...
Terrestrial cosmogenic nuclide (TCN) exposure dating has become the most dominant technique for cons...
Fluvial incision, regarded as one of the fundamental geomorphic processes, drives the evolution of m...
Global data suggest that erosion rates variously scale with steepness or climate forcing (precipitat...
The cosmogenic 10Be exposure histories of in situ bedrock surfaces from the Tibetan Plateau indicate...
The central Songpan–Ganzi belt, located on the eastern margin of the Tibetan Plateau, has a similar ...
Concentrations of in-situ-produced cosmogenic nuclides 10Be and 26Al in quartz were meas-ured by acc...
This paper builds a database of apatite fission track (AFT) ages and thermal-modeling results coveri...
Concentrations of in-situ-produced cosmogenic nuclides Be-10 and Al-26 in quartz were measured by ac...
International audienceThis contribution provides new constraints on the timing of Tibetan glacial re...
Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/94784/1/tect2305.pd
Quantifying long-term erosion rates across the Tibetan Plateau and its bordering mountains is of cri...
New detrital low-temperature thermochronometry provides estimates of long-term erosion rates and the...
The 5-km-high Tibetan plateau is an outstanding topographic feature on the earth today. Its areal ex...
Fluvial incision, regarded as one of the fundamental geomorphic processes, drives the evolution of m...
The Tibetan Plateau holds an ample record of past glaciations, and there is an extensive set of glac...
Terrestrial cosmogenic nuclide (TCN) exposure dating has become the most dominant technique for cons...
Fluvial incision, regarded as one of the fundamental geomorphic processes, drives the evolution of m...
Global data suggest that erosion rates variously scale with steepness or climate forcing (precipitat...