Articles | Volume 20, issue 11
https://doi.org/10.5194/cp-20-2399-2024
https://doi.org/10.5194/cp-20-2399-2024
Research article
 | 
04 Nov 2024
Research article |  | 04 Nov 2024

Rapid topographic growth of Diancang Shan, southeastern margin of the Tibetan Plateau, since 5.0–3.5 Ma

Chunxia Zhang, Haibin Wu, Xiuli Zhao, Yunkai Deng, Yunxia Jia, Wenchao Zhang, Shihu Li, and Chenglong Deng

Viewed

Total article views: 613 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
438 143 32 613 59 18 17
  • HTML: 438
  • PDF: 143
  • XML: 32
  • Total: 613
  • Supplement: 59
  • BibTeX: 18
  • EndNote: 17
Views and downloads (calculated since 18 Jun 2024)
Cumulative views and downloads (calculated since 18 Jun 2024)

Viewed (geographical distribution)

Total article views: 613 (including HTML, PDF, and XML) Thereof 623 with geography defined and -10 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 20 Nov 2024
Download
Short summary
Clarifying the paleoelevation changes of Diancang Shan (DCS) is important for comprehending both tectonics and the climatic effects in the transition zone between the high Tibetan Plateau and the lower relief of eastern and southern Asia. Our results show low elevations of DCS between ~ 7.6 and ~ 5.0 Ma, followed by significant uplift of 1000–2000 m between ~ 5.0 and ~ 3.5 Ma. They provide a novel method for reconstructing the paleoelevation of mountains like DCS in orogenic belts.