海原-六盘山地区活动构造的活动时间厘定: 来自光释光测年的限定

肖骏; 陈汉林; 林秀斌; Karl-HeinzWyrwoll; 王旭龙

doi:10.3799/dqkx.2011.105

Volume 36 Issue 6

Jun. 2011

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XIAO Jun, CHEN Han-lin, LIN Xiu-bin, Heinz Wyrwoll, WANG Xu-long, 2011. Determination of the Timing of Active Structures in Haiyuan-Liupan Shan Area: Constraints from OSL Dating. Earth Science, 36(6): 993-998. doi: 10.3799/dqkx.2011.105

Citation:

XIAO Jun, CHEN Han-lin, LIN Xiu-bin, Heinz Wyrwoll, WANG Xu-long, 2011. Determination of the Timing of Active Structures in Haiyuan-Liupan Shan Area: Constraints from OSL Dating. Earth Science, 36(6): 993-998. doi: 10.3799/dqkx.2011.105

Citation:

XIAO Jun, CHEN Han-lin, LIN Xiu-bin, Heinz Wyrwoll, WANG Xu-long, 2011. Determination of the Timing of Active Structures in Haiyuan-Liupan Shan Area: Constraints from OSL Dating. Earth Science, 36(6): 993-998. doi: 10.3799/dqkx.2011.105

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Determination of the Timing of Active Structures in Haiyuan-Liupan Shan Area: Constraints from OSL Dating

doi: 10.3799/dqkx.2011.105

XIAO Jun^{1, 2
,},
CHEN Han-lin^{1, 2
,
,},
LIN Xiu-bin^{1, 2, 3},
Heinz Wyrwoll³,
WANG Xu-long⁴

1.
Department of Earth Sciences, Zhejiang University, Hangzhou 310027, China
2.
Structural Research Center of Oil and Gas Bearing Basin, Ministry of Education, Hangzhou 310027, China
3.
School of Earth and Environment, The University of Western Australia, Stirling Highway, Crawley, WA 6009, Australia
4.
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China

Received Date: 2011-04-10
Available Online: 2021-11-10
Publish Date: 2011-06-15

Abstract

Abstract

Haiyuan-Liupan Shan area is located in the northeastern margin of present Tibetan plateau. The study of the active structures in this area will provide constraints not only for the seismic evaluation but also for the northeastward growth of the plateau. Based on the geological survey and optically stimulated luminescence (OSL) dating, the timing of the active structures has been determined. The results indicate that active structures occurred in Late Quaternary along the Haiyuan-Liupan Shan and Xiangshan-Tianjing Shan faults, forming the structures such as angular unconformity (planation surface), fold and fault. This suggests that Haiyuan-Liupan Shan area should be considered as a focus of seismic evaluation, and also that the Tibetan plateau grew in its northeast margin in Late Quaternary.
- Northeast Tibetan plateau,
- tectonics,
- active structure,
- optically stimulated luminescence (OSL)

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References(31)

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