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Volume 24 Issue 4
Aug 2013
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Article Contents
Zengbao Zhang, Chuanbo Shen, Chun Shao, Zhaoqian Liu. Tectonothermal Evolution of the Eastern Tibetan Plateau Foreland: Fission-Track Thermochronology of the Southern Dabashan Fold-Thrust Belt. Journal of Earth Science, 2013, 24(4): 479-490. doi: 10.1007/s12583-013-0344-z
Citation: Zengbao Zhang, Chuanbo Shen, Chun Shao, Zhaoqian Liu. Tectonothermal Evolution of the Eastern Tibetan Plateau Foreland: Fission-Track Thermochronology of the Southern Dabashan Fold-Thrust Belt. Journal of Earth Science, 2013, 24(4): 479-490. doi: 10.1007/s12583-013-0344-z

Tectonothermal Evolution of the Eastern Tibetan Plateau Foreland: Fission-Track Thermochronology of the Southern Dabashan Fold-Thrust Belt

doi: 10.1007/s12583-013-0344-z
Funds:

the National Natural Science Foundation of China 40902038

the PetroChina Innovation Foundation 2009D-5006-01-08

the Project of China Geological Survey 12120113094200

More Information
  • Corresponding author: Chuanbo Shen: cugshen@126.com
  • Received Date: 17 Sep 2012
  • Accepted Date: 23 Jan 2013
  • Publish Date: 01 Aug 2013
  • Apatite fission-track dating and thermal-history modeling were carried out on samples from the Dabashan (大巴山), a fold-thrust belt, northeast of the Sichuan (四川) Basin and east of the Tibetan Plateau. A first cooling event in the Late Cretaceous is followed by a prolonged period of thermal stability with exhumation rates of ≤0.025 mm/a, as determined from age vs. elevation relationships. The preservation of age vs. elevations relationships and the lack of distinct age changes across tectonic structures indicate that the Dabashan fold-thrust belt formed prior to the Late Cretaceous, consistent with the current view of Triassic-Early Cretaceous shortening. Relatively short mean track lengths (~12 μm) indicate that the samples remained in the partial annealing zone for a prolonged time. The knick points in the best-fitting temperature-time models suggest that the onset of late-stage accelerated cooling commenced at ≤11 Ma. Related exhumation rates are 0.3–0.2 mm/a assuming geothermal gradients of 20 and 30 ℃/km. We speculate that this late-stage event results from eastward growth of the Tibetan Plateau and overstepping of the Sichuan Basin, it is likely responsible for the youthful morphology of the Dabashan.

     

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