Richardson, N.J. and Densmore, A.L. and Seward, D. and Wipf, M. and Li, Y. and Ellis, M.A. and Zhang, Y. (2008) 'Extraordinary denudation in the Sichuan Basin : insights from low-temperature thermochronology adjacent to the eastern margin of the Tibetan Plateau.', Journal of geophysical research : solid earth., 113 (B4). B04409.
The eastern margin of the Tibetan Plateau combines very high relief with almost no Tertiary foreland sedimentation and little evidence of Cenozoic tectonic shortening. While river incision and landscape development at the plateau margin have received significant attention over the last decade, little is known about the Cenozoic development of the adjacent Sichuan Basin. Here we assess the Cenozoic thermal history of this basin using detrital apatite fission track (AFT) and (U-Th)/He techniques and establish the presence of an exhumed AFT paleopartial annealing zone across much of the basin. This observation, combined with stratigraphic and borehole sections and inverse modeling of confined apatite fission tracks, indicates that the strata within the basin have undergone accelerated cooling after similar to 40 Ma, consistent with the widespread erosion of similar to 1 to 4 km of overlying sedimentary material. This regional-scale erosion is most likely a response to changes in the Yangtze River system draining and removing sediment from the basin. The base-level fall associated with this erosion contributed to a relative increase in relief across the Longmen Shan and may have helped drive Miocene-Recent incision and unloading of the plateau margin.
|Keywords:||Thermochronology, Sichuan Basin, Yangtze, Tibet, Longmen Shan.|
|Full text:||PDF - Published Version (1816Kb)|
|Publisher Web site:||http://dx.doi.org/10.1029/2006JB004739|
|Publisher statement:||© 2008 American Geophysical Union. Richardson, N. J. and Densmore, A. L. and Seward, D. and Wipf, M. and Li, Y. and Ellis, M. A. and Zhang, Y., (2008), 'Extraordinary denudation in the Sichuan Basin : insights from lowtemperature thermochronology adjacent to the eastern margin of the Tibetan Plateau.', Journal of geophysical research : solid earth., 113, B04409, 10.1029/2006JB004739. To view the published open abstract, go to http://dx.doi.org and enter the DOI.|
|Record Created:||06 Oct 2008|
|Last Modified:||31 Jul 2015 14:36|
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