Articles | Volume 10, issue 4
https://doi.org/10.5194/se-10-1355-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-10-1355-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
20 Aug 2019
Research article | Highlight paper |
| 20 Aug 2019
| 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
CORRESPONDING AUTHOR
NEXT – Natural and Experimental Tectonics Research Group – Department
of Chemistry, Life Sciences and Environmental Sustainability, University of
Parma, Italy
Rudy Swennen
Department of Earth and Environmental Sciences, KU Leuven, Leuven, Belgium
Fabrizio Balsamo
NEXT – Natural and Experimental Tectonics Research Group – Department
of Chemistry, Life Sciences and Environmental Sustainability, University of
Parma, Italy
Hamdy El Desouky
Department of Earth and Environmental Sciences, KU Leuven, Leuven, Belgium
Geology Department, Faculty of Science, Menoufia University, Menoufia,
Egypt
Fabrizio Storti
NEXT – Natural and Experimental Tectonics Research Group – Department
of Chemistry, Life Sciences and Environmental Sustainability, University of
Parma, Italy
Conxita Taberner
Shell Global Solutions International B.V., Amsterdam, the Netherlands
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Cited
17 citations as recorded by crossref.
- Fault-controlled saddle dolomitization during the late Triassic Pangea breakup in the southern Adria domain (Southern Italy) R. Diamanti et al. 10.1016/j.marpetgeo.2024.107216
- How the geochemistry of syn-kinematic calcite cement depicts past fluid flow and assists structural interpretations: a review of concepts and applications in orogenic forelands N. Beaudoin et al. 10.1017/S0016756822001327
- Evaluation of fault and fracture controlled hydrothermal dolomitization in the Jurassic carbonate succession of the lesser Himalayas, NW Pakistan H. Rahim et al. 10.1007/s13146-025-01059-3
- Rift and salt-related multi-phase dolomitization: example from the northwestern Pyrenees G. Motte et al. 10.1016/j.marpetgeo.2021.104932
- Micro‐scale chemical and physical patterns in an interface of hydrothermal dolomitization reveals the governing transport mechanisms in nature: Case of the Layens anticline, Pyrenees, France S. Centrella et al. 10.1111/sed.12808
- Regional-scale paleofluid system across the Tuscan Nappe–Umbria–Marche Apennine Ridge (northern Apennines) as revealed by mesostructural and isotopic analyses of stylolite–vein networks N. Beaudoin et al. 10.5194/se-11-1617-2020
- Along- and across-strike variation of damage zone parameters in the Kornos-Aghios Ioannis normal fault, Lemnos Island, Greece L. Berio et al. 10.1016/j.jsg.2023.104981
- Estimating the fluid composition after dolomitization using mass balance equation: comparison of examples from Spain, Canada and France S. Centrella et al. 10.1016/j.gloplacha.2022.104016
- The Fault Effects on the Oil Migration in the Ultra-Deep Fuman Oilfield of the Tarim Basin, NW China Y. Zhu et al. 10.3390/en15165789
- Persisting Rock-Buffered Conditions in the Upper Triassic and Lower Jurassic Dolomites of the Central Apennines (Italy) During Diagenesis, Burial, and Thrusting A. Lucca et al. 10.3390/geosciences15020035
- Dolomitization mechanism of Pila Spi formation (middle- late eocene) in the high folded zone, Northern Iraq R. Ali 10.1016/j.kjs.2023.02.015
- Influence of basement rocks on fluid evolution during multiphase deformation: the example of the Estamariu thrust in the Pyrenean Axial Zone D. Muñoz-López et al. 10.5194/se-11-2257-2020
- Dolomite luminescence thermochronometry reconstructs the low-temperature exhumation history of carbonate rocks in the central Apennines, Italy J. Zhang et al. 10.1038/s43247-025-02216-1
- Hydrothermal alteration and hydrocarbon accumulations in ultra-deep carbonate reservoirs along a strike-slip fault system, Tarim Basin, NW China J. Su et al. 10.1016/j.petrol.2021.108605
- Hydrothermal activity and its influence on hydrocarbon accumulation in deep dolomite reservoirs of the Ediacaran Dengying Formation, Sichuan Basin Z. Wang et al. 10.1016/j.engeos.2024.100370
- Dinaric up-thrusts in the Pliocene evolution of the Central Apennines thrust belt of Italy: the Montagna dei Fiori structure F. Calamita et al. 10.1017/S0016756821000613
- From Early Contraction to Post-Folding Fluid Evolution in the Frontal Part of the Bóixols Thrust Sheet (Southern Pyrenees) as Revealed by the Texture and Geochemistry of Calcite Cements N. Nardini et al. 10.3390/min9020117
16 citations as recorded by crossref.
- Fault-controlled saddle dolomitization during the late Triassic Pangea breakup in the southern Adria domain (Southern Italy) R. Diamanti et al. 10.1016/j.marpetgeo.2024.107216
- How the geochemistry of syn-kinematic calcite cement depicts past fluid flow and assists structural interpretations: a review of concepts and applications in orogenic forelands N. Beaudoin et al. 10.1017/S0016756822001327
- Evaluation of fault and fracture controlled hydrothermal dolomitization in the Jurassic carbonate succession of the lesser Himalayas, NW Pakistan H. Rahim et al. 10.1007/s13146-025-01059-3
- Rift and salt-related multi-phase dolomitization: example from the northwestern Pyrenees G. Motte et al. 10.1016/j.marpetgeo.2021.104932
- Micro‐scale chemical and physical patterns in an interface of hydrothermal dolomitization reveals the governing transport mechanisms in nature: Case of the Layens anticline, Pyrenees, France S. Centrella et al. 10.1111/sed.12808
- Regional-scale paleofluid system across the Tuscan Nappe–Umbria–Marche Apennine Ridge (northern Apennines) as revealed by mesostructural and isotopic analyses of stylolite–vein networks N. Beaudoin et al. 10.5194/se-11-1617-2020
- Along- and across-strike variation of damage zone parameters in the Kornos-Aghios Ioannis normal fault, Lemnos Island, Greece L. Berio et al. 10.1016/j.jsg.2023.104981
- Estimating the fluid composition after dolomitization using mass balance equation: comparison of examples from Spain, Canada and France S. Centrella et al. 10.1016/j.gloplacha.2022.104016
- The Fault Effects on the Oil Migration in the Ultra-Deep Fuman Oilfield of the Tarim Basin, NW China Y. Zhu et al. 10.3390/en15165789
- Persisting Rock-Buffered Conditions in the Upper Triassic and Lower Jurassic Dolomites of the Central Apennines (Italy) During Diagenesis, Burial, and Thrusting A. Lucca et al. 10.3390/geosciences15020035
- Dolomitization mechanism of Pila Spi formation (middle- late eocene) in the high folded zone, Northern Iraq R. Ali 10.1016/j.kjs.2023.02.015
- Influence of basement rocks on fluid evolution during multiphase deformation: the example of the Estamariu thrust in the Pyrenean Axial Zone D. Muñoz-López et al. 10.5194/se-11-2257-2020
- Dolomite luminescence thermochronometry reconstructs the low-temperature exhumation history of carbonate rocks in the central Apennines, Italy J. Zhang et al. 10.1038/s43247-025-02216-1
- Hydrothermal alteration and hydrocarbon accumulations in ultra-deep carbonate reservoirs along a strike-slip fault system, Tarim Basin, NW China J. Su et al. 10.1016/j.petrol.2021.108605
- Hydrothermal activity and its influence on hydrocarbon accumulation in deep dolomite reservoirs of the Ediacaran Dengying Formation, Sichuan Basin Z. Wang et al. 10.1016/j.engeos.2024.100370
- Dinaric up-thrusts in the Pliocene evolution of the Central Apennines thrust belt of Italy: the Montagna dei Fiori structure F. Calamita et al. 10.1017/S0016756821000613
Discussed (preprint)
Latest update: 07 Jun 2025
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.
The dolomitized intervals of the Lower Jurassic deposits exposed in the Montagna dei Fiori...
