TISSION-TRACK DATING FOR ACTIVITY OF THE LONGMENSHAN FAULT ZONE AND UPLIFTING OF THE WESTERN SICHUAN PLATEAU

YANG Nong; ZHANG Yueqiao

Volume 16 Issue 4

Dec. 2010

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Article Navigation > Journal of Geomechanics > 2010 > 16(4): 359-371

Liu Gengnian, Cui Zhijiu, Wu Yongqiu, et al., 1997. RECORD OF ENVIRONMENTAL CHANGE IN RESHUI PROFILE AT KUNLUNSHAN PASS SINCE 18 kaBP. Journal of Geomechanics, 3 (4): 39-45.

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YANG Nong, ZHANG Yueqiao, 2010. TISSION-TRACK DATING FOR ACTIVITY OF THE LONGMENSHAN FAULT ZONE AND UPLIFTING OF THE WESTERN SICHUAN PLATEAU. Journal of Geomechanics, 16 (4): 359-371.

Liu Gengnian, Cui Zhijiu, Wu Yongqiu, et al., 1997. RECORD OF ENVIRONMENTAL CHANGE IN RESHUI PROFILE AT KUNLUNSHAN PASS SINCE 18 kaBP. Journal of Geomechanics, 3 (4): 39-45.

Citation:

YANG Nong, ZHANG Yueqiao, 2010. TISSION-TRACK DATING FOR ACTIVITY OF THE LONGMENSHAN FAULT ZONE AND UPLIFTING OF THE WESTERN SICHUAN PLATEAU. Journal of Geomechanics, 16 (4): 359-371.

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TISSION-TRACK DATING FOR ACTIVITY OF THE LONGMENSHAN FAULT ZONE AND UPLIFTING OF THE WESTERN SICHUAN PLATEAU

YANG Nong^{1, 2},
ZHANG Yueqiao^{1, 2}

1.
Key Laboratory of Neotectonic Movement and Geohazard, Ministry of Land and Resources, Beijing, 100081, China
2.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, 100081, China

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Abstract

Abstract

Twelve samples of tectonites, metasediments and granites taken from the western Sichuan Plateau were dated in this study by apatite fission track dating method. The results are used to reconstruct uplifting history and fault activity of the Longmenshan tectonic belt in eastern margin of the Tibetan Plateau. It is shown that the recent activity of the two major boundary faults:the Wenchuan-Maowen fault and the Yingxiu-Beichuan fault, occurred in early Pleistocene (FT ages of 1.2~1.3 Ma); the Miyaluo fault developed in the interior of the plateau was strongly active in middle Pleistocene (around 0.5 Ma); the back Longmenshan tectonic zone started to uplift in Miocene; and the interior of the plateau began rapid uplift in latest Pliocene to Middle Pleistocene. The uplifting of the plateau caused formation of deep-incised river morphology.
- Late Cenozoic,
- western Sichuan Plateau,
- Longmenshan fault zone,
- Uplift,
- apatite fission track dating

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References(42)

References

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TISSION-TRACK DATING FOR ACTIVITY OF THE LONGMENSHAN FAULT ZONE AND UPLIFTING OF THE WESTERN SICHUAN PLATEAU

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TISSION-TRACK DATING FOR ACTIVITY OF THE LONGMENSHAN FAULT ZONE AND UPLIFTING OF THE WESTERN SICHUAN PLATEAU

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