Articles | Volume 10, issue 4
https://doi.org/10.5194/se-10-1355-2019
https://doi.org/10.5194/se-10-1355-2019
Research article
 | Highlight paper
 | 
20 Aug 2019
Research article | Highlight paper |  | 20 Aug 2019

Fault-controlled dolomitization in the Montagna dei Fiori Anticline (Central Apennines, Italy): record of a dominantly pre-orogenic fluid migration

Mahtab Mozafari, Rudy Swennen, Fabrizio Balsamo, Hamdy El Desouky, Fabrizio Storti, and Conxita Taberner

Viewed

Total article views: 5,107 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
3,972 999 136 5,107 130 128
  • HTML: 3,972
  • PDF: 999
  • XML: 136
  • Total: 5,107
  • BibTeX: 130
  • EndNote: 128
Views and downloads (calculated since 03 Jan 2019)
Cumulative views and downloads (calculated since 03 Jan 2019)

Viewed (geographical distribution)

Total article views: 5,107 (including HTML, PDF, and XML) Thereof 3,974 with geography defined and 1,133 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (preprint)

Latest update: 29 Jun 2024
Download
Short summary
The dolomitized intervals of the Lower Jurassic deposits exposed in the Montagna dei Fiori Anticline (Central Apennines, Italy) have been investigated. Accordingly, two fault-related dolomitization events were recognised and interpreted as having occurred before and during the Apenninic orogeny. The analyses suggest significant involvement of evaporitic fluids in both events, most likely derived from the underlying Upper Triassic Burano Formation in the detachment level.