Onset timing of significant unroofing around Qaidam basin, northern Tibet, China: Constraints from 40Ar/39Ar and FT thermochronology on granitoids

Fei Wang, Ching Hua Lo, Qi Li, Meng Wan Yeh, Jinglin Wan, Dewen Zheng, Erqi Wang

Research output: Contribution to journalArticle

84 Citations (Scopus)

Abstract

40Ar/39Ar and fission track thermochronological results from two granitoid suites in the mountain ranges along the northern and southern edges of Qaidam basin constrain the timing of a Tertiary denudation event and their tectonic association in northern Tibet. The cooling histories based upon 40Ar/ 39Ar and fission track ages suggest a rapid cooling event (7.5-10.7 °C/Ma) during Oligocene-early Miocene time. This cooling event is thought to reflect an increasing denudation rate associated with the rapid uplift and denudation of the North Qaidam and Kunlun Shan mountain ranges. With consideration to the field evidence, sedimentation rate of the Qaidam basin, and the propagation rate along the Altyn Tagh fault, the rapid uplifting and denudation are probably due to crustal thickening associated with Cenozoic propagation of the Altyn Tagh fault in accommodating the collision of India with Asia.

Original languageEnglish
Pages (from-to)59-69
Number of pages11
JournalJournal of Asian Earth Sciences
Volume24
Issue number1
DOIs
Publication statusPublished - 2004 Oct

Fingerprint

thermochronology
unroofing
denudation
cooling
basin
crustal thickening
granitoid
sedimentation rate
Oligocene
collision
uplift
Miocene
tectonics
history
rate
mountain range

Keywords

  • Fission track dating
  • Multi-domain diffusion model
  • Qaidam basin
  • Unroofing

ASJC Scopus subject areas

  • Geology
  • Earth-Surface Processes

Cite this

Onset timing of significant unroofing around Qaidam basin, northern Tibet, China : Constraints from 40Ar/39Ar and FT thermochronology on granitoids. / Wang, Fei; Lo, Ching Hua; Li, Qi; Yeh, Meng Wan; Wan, Jinglin; Zheng, Dewen; Wang, Erqi.

In: Journal of Asian Earth Sciences, Vol. 24, No. 1, 10.2004, p. 59-69.

Research output: Contribution to journalArticle

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abstract = "40Ar/39Ar and fission track thermochronological results from two granitoid suites in the mountain ranges along the northern and southern edges of Qaidam basin constrain the timing of a Tertiary denudation event and their tectonic association in northern Tibet. The cooling histories based upon 40Ar/ 39Ar and fission track ages suggest a rapid cooling event (7.5-10.7 °C/Ma) during Oligocene-early Miocene time. This cooling event is thought to reflect an increasing denudation rate associated with the rapid uplift and denudation of the North Qaidam and Kunlun Shan mountain ranges. With consideration to the field evidence, sedimentation rate of the Qaidam basin, and the propagation rate along the Altyn Tagh fault, the rapid uplifting and denudation are probably due to crustal thickening associated with Cenozoic propagation of the Altyn Tagh fault in accommodating the collision of India with Asia.",
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AB - 40Ar/39Ar and fission track thermochronological results from two granitoid suites in the mountain ranges along the northern and southern edges of Qaidam basin constrain the timing of a Tertiary denudation event and their tectonic association in northern Tibet. The cooling histories based upon 40Ar/ 39Ar and fission track ages suggest a rapid cooling event (7.5-10.7 °C/Ma) during Oligocene-early Miocene time. This cooling event is thought to reflect an increasing denudation rate associated with the rapid uplift and denudation of the North Qaidam and Kunlun Shan mountain ranges. With consideration to the field evidence, sedimentation rate of the Qaidam basin, and the propagation rate along the Altyn Tagh fault, the rapid uplifting and denudation are probably due to crustal thickening associated with Cenozoic propagation of the Altyn Tagh fault in accommodating the collision of India with Asia.

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