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Extraordinary denudation in the Sichuan Basin: insights from low-temperature thermochronology adjacent to the eastern margin of the Tibetan Plateau

Richardson, N.J.; Densmore, A.L.; Seward, D.; Wipf, M.; Li, Y.; Ellis, M.A.; Zhang, Y.

Extraordinary denudation in the Sichuan Basin: insights from low-temperature thermochronology adjacent to the eastern margin of the Tibetan Plateau Thumbnail


Authors

N.J. Richardson

D. Seward

M. Wipf

Y. Li

M.A. Ellis

Y. Zhang



Abstract

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.

Citation

Richardson, N., Densmore, A., Seward, D., Wipf, M., Li, Y., Ellis, M., & 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, 113(B4), Article B04409. https://doi.org/10.1029/2006jb004739

Journal Article Type Article
Publication Date Apr 17, 2008
Deposit Date Oct 6, 2008
Publicly Available Date Mar 23, 2010
Journal Journal of Geophysical Research. Solid Earth
Print ISSN 0148-0227
Electronic ISSN 2156-2202
Publisher Wiley
Peer Reviewed Peer Reviewed
Volume 113
Issue B4
Article Number B04409
DOI https://doi.org/10.1029/2006jb004739
Keywords Thermochronology, Sichuan Basin, Yangtze, Tibet, Longmen Shan.
Public URL https://durham-repository.worktribe.com/output/1574802

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Copyright 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.






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