ORCID Profile
0000-0002-9531-7208
Current Organisation
Guangzhou Institute of Geochemistry, Chinese Academy of Sciences
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Publisher: Elsevier BV
Date: 09-2010
Publisher: Elsevier BV
Date: 07-2011
Publisher: American Journal of Science (AJS)
Date: 2014
DOI: 10.2475/01.2014.09
Publisher: Elsevier BV
Date: 05-2016
Publisher: Elsevier BV
Date: 08-2015
Publisher: Geological Society of America
Date: 09-2010
DOI: 10.1130/B30007.1
Publisher: Elsevier BV
Date: 06-2015
Publisher: Springer Science and Business Media LLC
Date: 14-09-2017
Publisher: Elsevier BV
Date: 12-2004
Publisher: Elsevier BV
Date: 2012
Publisher: American Geophysical Union (AGU)
Date: 11-2018
DOI: 10.1029/2018JB015495
Publisher: Wiley
Date: 25-04-2017
DOI: 10.1111/TER.12265
Publisher: Elsevier BV
Date: 04-2017
Publisher: Oxford University Press (OUP)
Date: 07-2016
Publisher: Elsevier BV
Date: 03-2018
Publisher: Springer Science and Business Media LLC
Date: 09-01-2023
Publisher: Elsevier BV
Date: 06-2017
Publisher: American Geophysical Union (AGU)
Date: 10-2018
DOI: 10.1029/2018TC005170
Publisher: Elsevier BV
Date: 09-2016
Publisher: American Geophysical Union (AGU)
Date: 10-2020
DOI: 10.1029/2020JB020673
Publisher: Elsevier BV
Date: 10-2010
Publisher: Elsevier BV
Date: 10-2023
Publisher: Elsevier BV
Date: 10-2010
Publisher: Elsevier BV
Date: 11-2016
Publisher: Oxford University Press (OUP)
Date: 11-06-2010
Publisher: Elsevier BV
Date: 09-2018
Publisher: American Geophysical Union (AGU)
Date: 26-04-2023
DOI: 10.1029/2022GL102700
Abstract: The East Kunlun Shan (EKLS) in northern Tibet occupies boundaries of the low‐relief topography and lower crustal low‐velocity zone in the interior plateau, making it ideal for exploring the relationship of surface deformation with underlying geodynamic processes. We used previous and new apatite (U‐Th)/He data to analyze the exhumation history and pattern throughout the EKLS and link surface deformation to deep structures. Integrated (U‐Th)/He ages reveal the rapid exhumation at 27–25 Ma, due to the coeval orogen‐scale tilting of the EKLS. Along with the crustal structures beneath the EKLS, it is inferred that orogen‐scale tilting is the isostatic response of the nonuniform crustal thickening related to northward injection of the Tibetan lower crust. This study highlights the role of ductile deformation within the lower crust in mountain building in northern Tibet, which shares a similarity with mountain building pattern in the eastern plateau margin.
Location: China
Location: No location found
No related grants have been discovered for Yigang Xu.