We document a permeable step-over zone in a normal fault setting. • Meters-thick (6,5 m) banded Ca-carbonate veins filled the fractures in the step-over zone. • We describe the root of an hydrothermal system feeding travertine deposits. • Fissure ridge-type travertine deposits are related to the step-over zone.
Step-over fault zones controlling geothermal fluid-flow and travertine formation (Denizli Basin, Turkey) / Brogi, Andrea; Alçiçek, M. Cihat; Liotta, Domenico; Capezzuoli, Enrico; Zucchi, Martina; Matera, Paola Francesca. - In: GEOTHERMICS. - ISSN 0375-6505. - ELETTRONICO. - 89:(2021), pp. 101941-101950. [10.1016/j.geothermics.2020.101941]
Step-over fault zones controlling geothermal fluid-flow and travertine formation (Denizli Basin, Turkey)
Capezzuoli, EnricoSupervision
;
2021
Abstract
We document a permeable step-over zone in a normal fault setting. • Meters-thick (6,5 m) banded Ca-carbonate veins filled the fractures in the step-over zone. • We describe the root of an hydrothermal system feeding travertine deposits. • Fissure ridge-type travertine deposits are related to the step-over zone.
| File | Dimensione | Formato | |
|---|---|---|---|
|
Brogi et alii, 2021 (Geothermics) copia.pdf
Accesso chiuso
Tipologia:
Pdf editoriale (Version of record)
Licenza:
Solo lettura
Dimensione
2.97 MB
Formato
Adobe PDF
|
2.97 MB | Adobe PDF | Richiedi una copia |
I documenti in FLORE sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
