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Cited by 1,171

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Present-Day Crustal Deformation in China Constrained by Global Positioning System Measurements

Wang, Qi, Zhang, Pei-Zhen, Freymueller, Jeffrey T., Bilham, Roger, Larson, Kristine M., Lai, Xi'an, You, Xinzhao, Niu, Zhijun, Wu, Jianchun, Li, Yanxin, Liu, Jingnan, Yang, Zhiqiang, Chen, Qizhi·2001·Science

Abstract

Global Positioning System (GPS) measurements in China indicate that crustal shortening accommodates most of India's penetration into Eurasia. Deformation within the Tibetan Plateau and its margins, the Himalaya, the Altyn Tagh, and the Qilian Shan, absorbs more than 90% of the relative motion between the Indian and Eurasian plates. Internal shortening of the Tibetan plateau itself accounts for more than one-third of the total convergence. However, the Tibetan plateau south of the Kunlun and Ganzi-Mani faults is moving eastward relative to both India and Eurasia. This movement is accommodated through rotation of material around the eastern Syntaxis. The North China and South China blocks, east of the Tibetan Plateau, move coherently east-southeastward at rates of 2 to 8 millimeters per year and 6 to 11 millimeters per year, respectively, with respect to the stable Eurasia.

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Metadata

Authors
Wang, Q., Zhang, P.-Z., Freymueller, J. T., Bilham, R., Larson, K. M., Lai, X., You, X., Niu, Z., Wu, J., Li, Y., Liu, J., Yang, Z., & Chen, Q.
Venue
Science
Published
2001-10-19
Volume
294
Issue
5542
Pages
574-577
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2171223935
Cited by
1,171
References
0
FWCI
40.11
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Present-Day Crustal Deformation in China Constrained by Global Positioning System Measurements. https://app.cochat.ai/papers/10.1126/science.1063647
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Wang, Q., Zhang, P.-Z., Freymueller, J. T., Bilham, R., Larson, K. M., Lai, X., You, X., Niu, Z., Wu, J., Li, Y., Liu, J., Yang, Z., & Chen, Q. (2001). Present-Day Crustal Deformation in China Constrained by Global Positioning System Measurements. Science. https://doi.org/10.1126/science.1063647

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