嘉黎断裂带两侧晚新生代差异隆升的磷灰石裂变径迹纪录

向树元民; 马新民; 泽仁扎西; 巴桑次仁

Volume 32 Issue 5

Sep. 2007

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Article Navigation > Earth Science > 2007 > 32(5): 615-621

XIANG Shu-yuan-min, MA Xin-min, ZE Ren-zha-xi, BA Sang-ci-ren, 2007. Record of Apatite Fission Track of the Differential Uplift in Both Sides of Jiali Fault Belt since Late Cenozoic. Earth Science, 32(5): 615-621.

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Record of Apatite Fission Track of the Differential Uplift in Both Sides of Jiali Fault Belt since Late Cenozoic

1.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
North west Branch of the Research Institute of Petroleum Exploration and Development , Petro China, Lanzhou 730020, China
3.
Institute of Geology Survey of Tibet Autonomous Region , Lhasa 850007, China

Received Date: 2007-06-16
Publish Date: 2007-09-25

Abstract

Abstract

The apatite fission track (AFT) chronology in both sides of Jiali fault belt shows that the AFT age in the north side of the fault belt is 5.6-11.7 Ma which belongs to Late Miocene; and the age of the south side is obviously younger, because the ages of five out of six samples are between 4.0 Ma and 5.9 Ma, belonging to early Pliocene. During 5.6-11.7 Ma, the uplift rate in the north side of Jiali fault belt is 0.07-0.09 mm/a. Since 5.8 Ma, the average denudation rate is 0.50 mm/a, and the average uplift rate is 1.33 mm/a in the north side. While, the average rate of denudation and uplift is 0.62 mm/a and 1.68 mm/a in the south side of Jiali fault belt since 4.7 Ma. The samples collected from both sides of Jiali fault belt reflect the strong uplift since Pliocene, and the south side uplifts more strongly than the north side.
- Jiali fault belt,
- late Cenozoic,
- apatite fission track,
- plateau uplift

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Record of Apatite Fission Track of the Differential Uplift in Both Sides of Jiali Fault Belt since Late Cenozoic

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