Yongjun Yue, Ph.D.
Affiliations: | 2003 | Stanford University, Palo Alto, CA |
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GeologyGoogle:
"Yongjun Yue"Parents
Sign in to add mentorStephan Alan Graham | grad student | 2003 | Stanford | |
(Slip history of the Altyn Tagh fault and its implications for tectonics of Asia.) |
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Publications
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Ritts BD, Yue Y, Graham SA, et al. (2008) From sea level to high elevation in 15 million years:Uplift history of the northern Tibetan Plateau margin in the Altun Shan American Journal of Science. 308: 657-678 |
Yue Y, Graham SA, Ritts BD, et al. (2005) Detrital zircon provenance evidence for large-scale extrusion along the Altyn Tagh fault Tectonophysics. 406: 165-178 |
Darby BJ, Ritts BD, Yue Y, et al. (2005) Did the Altyn Tagh fault extend beyond the Tibetan Plateau Earth and Planetary Science Letters. 240: 425-435 |
Ritts BD, Yue Y, Graham SA. (2004) Oligocene-Miocene tectonics and sedimentation along the Altyn Tagh fault, northern Tibetan Plateau: Analysis of the Xorkol, Subei, and Aksay basins Journal of Geology. 112: 207-229 |
Yue Y, Ritts BD, Graham SA, et al. (2004) Slowing extrusion tectonics: lowered estimate of post-Early Miocene slip rate for the Altyn Tagh fault Earth and Planetary Science Letters. 217: 111-122 |
Yue Y, Ritts BD, Hanson AD, et al. (2004) Sedimentary evidence against large strike-slip translation on the Northern Altyn Tagh fault, NW China Earth and Planetary Science Letters. 228: 311-323 |
Yue Y, Liou JG, Graham SA. (2001) Tectonic correlation of Beishan and Inner Mongolia orogens and its implications for the palinspastic reconstruction of north China Memoir of the Geological Society of America. 194: 101-116 |
Yue Y, Ritts BD, Graham SA. (2001) Initiation and Long-Term Slip History of the Altyn Tagh Fault International Geology Review. 43: 1087-1093 |
Yue Y, Liou JG. (1999) Two-stage evolution model for the Altyn Tagh fault, China Geology. 27: 227-230 |
Ritts BD, Bovet PM, Kent-Corson ML, et al. (1970) Structural, paleogeographic and topographic evolution of the northern Tibetan Plateau margin: Evidence from the southern Tarim basin, northern Hexi Corridor, and Qaidam basin Himalayan Journal of Sciences. 5: 121-122 |