Travertine deposits constraining transfer zone neotectonics in geothermal areas: An example from the inner Northern Apennines (Bagno Vignoni-Val d’Orcia area, Italy)

Travertine deposits constraining transfer zone neotectonics in geothermal areas: An example from the inner Northern Apennines (Bagno Vignoni-Val d’Orcia area, Italy)

•Transfer zones play as permeable volumes channeling geothermal fluids.•Travertine deposition is coeval with faulting.•Travertine deposits are useful tools to reconstruct the activity of faults.•The Bagno Vignoni geothermal area is located along active fault segments.•Earthquakes with M 

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Veröffentlicht in:Geothermics 2020-05, Vol.85, p.101763-22, Article 101763
Hauptverfasser: Brogi, Andrea, Liotta, Domenico, Capezzuoli, Enrico, Matera, Paola Francesca, Kele, Sándor, Soligo, Michele, Tuccimei, Paola, Ruggieri, Giovanni, Yu, Tsai-Luen, Shen, Chuan-Chou, Huntington, Katharine W.
Format: Artikel
Sprache:eng
Schlagworte:
Calcite
Deposits
Extensional tectonics
Fault lines
Geological faults
Geothermal areas
Geothermal power
Holocene
Hot springs
Isotopes
Kinematics
Low-Temperature geothermal areas
Magma
Miocene
Neotectonics
Plate tectonics
Pleistocene
Quarries
Seismicity
Seismotectonic setting
Shear zone
Tectonic activity
Tectonics
Travertine
Veins (geology)
Veins (plant anatomy)
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Beschreibung
Zusammenfassung:•Transfer zones play as permeable volumes channeling geothermal fluids.•Travertine deposition is coeval with faulting.•Travertine deposits are useful tools to reconstruct the activity of faults.•The Bagno Vignoni geothermal area is located along active fault segments.•Earthquakes with M 
ISSN:0375-6505
1879-3576
DOI:10.1016/j.geothermics.2019.101763