Solid Earth
Solid Earth
SE
Articles | Volume 16, issue 7
Articles | Volume 16, issue 7
https://doi.org/10.5194/se-16-663-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-16-663-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 16, issue 7
Research article
 | 
14 Jul 2025
Research article |  | 14 Jul 2025

What do arc magmatism trace-element patterns and Sr–Nd–Pb isotopic data reflect? Insights from the Urumieh–Dokhtar magmatic arc of Iran

Mohammad Reza Ghorbani, Meysam Akbari, Ian T. Graham, Mathieu Benoit, and Fatemeh Sepidbar

Viewed

Total article views: 501 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
313 119 69 501 36 23 33
  • HTML: 313
  • PDF: 119
  • XML: 69
  • Total: 501
  • Supplement: 36
  • BibTeX: 23
  • EndNote: 33
Views and downloads (calculated since 19 Nov 2024)
Cumulative views and downloads (calculated since 19 Nov 2024)

Viewed (geographical distribution)

Total article views: 501 (including HTML, PDF, and XML) Thereof 501 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 15 Jul 2025
Download
Short summary
The vast Cenozoic arc magmatism of Iran introduced three distinct rock series. The LILE (large-ion lithophile elements)-rich and LILE-poor series show signatures of fluid-rich and fluid-poor slab-melt mantle metasomatism, furnished by hot slab subduction. The slab was more hydrated in the northern segment of the study area, where the LILE-rich series dominates. The third series rich in incompatible trace elements, the ITE-rich series, indicates the input of asthenosphere as well.
Read more
Share