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Solid Earth An interactive open-access journal of the European Geosciences Union
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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.
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SE | Articles | Volume 10, issue 4
SE | Articles | Volume 10, issue 4
Solid Earth, 10, 1355–1383, 2019
https://doi.org/10.5194/se-10-1355-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
Solid Earth, 10, 1355–1383, 2019
https://doi.org/10.5194/se-10-1355-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
SE | Articles | Volume 10, issue 4

Research article 20 Aug 2019

Research article | 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 et al.

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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.
Read more
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Solid Earth

An interactive open-access journal of the European Geosciences Union

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