Articles | Volume 10, issue 1
https://doi.org/10.5194/se-10-149-2019
https://doi.org/10.5194/se-10-149-2019
Research article
 | 
18 Jan 2019
Research article |  | 18 Jan 2019

Tectono-thermal evolution of Oman's Mesozoic passive continental margin under the obducting Semail Ophiolite: a case study of Jebel Akhdar, Oman

Arne Grobe, Christoph von Hagke, Ralf Littke, István Dunkl, Franziska Wübbeler, Philippe Muchez, and Janos L. Urai

Viewed

Total article views: 4,109 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,720 1,273 116 4,109 485 131 118
  • HTML: 2,720
  • PDF: 1,273
  • XML: 116
  • Total: 4,109
  • Supplement: 485
  • BibTeX: 131
  • EndNote: 118
Views and downloads (calculated since 14 Aug 2018)
Cumulative views and downloads (calculated since 14 Aug 2018)

Viewed (geographical distribution)

Total article views: 4,109 (including HTML, PDF, and XML) Thereof 3,489 with geography defined and 620 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Discussed (preprint)

Latest update: 03 Nov 2024
Download
Short summary
The Mesozoic sequences of the Oman mountains experienced only weak post-obduction overprint and deformation, and thus they offer a unique natural laboratory to study obduction. We present a study of pressure and temperature evolution in the passive continental margin under the Oman Ophiolite using numerical basin models calibrated with thermal maturity data, fluid-inclusion thermometry, and low-temperature thermochronology.