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Composition and evolution of fluids during skarn development in the Monte Capanne thermal aureole, Elba Island, central Italy.

Autor: ROSSETTI, F.¹, TECCE, F.² francesca.tecce@igag.cnr.it

Publikováno v: Geofluids. Aug2008, Vol. 8 Issue 3, p167-180. 14p. 5 Diagrams, 2 Graphs, 1 Map.

travertine deposits at Semproniano, southern Tuscany, Italy: Estimate of

Autor: Berardi, G, Vignaroli, G, Billi, A, Rossetti, F, Soligo, M, Kele, S, Baykara, MO, Bernasconi, SM, Castorina, F, Tecce, F, Shen, CC

A giant carbonate vein (>= 50 m thick; fissure ridge travertines) and nearby travertine plateaus in the Semproniano area (Mt. Amiata geothermal field, southern Tuscany, Italy) are investigated through a multidisciplinary approach, including field and

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::48b152389d8a21032e66cb1edc339817
http://acikerisim.pau.edu.tr:8080/xmlui/handle/11499/15374

Paleoclimate reconstruction during the Messinian evaporative drawdown of the Mediterranean Basin: Insights from microthermometry on halite fluid inclusions

Autor: SPERANZA G., TECCE F., COSENTINO, Domenico, FACCENNA, CLAUDIO

Publikováno v: Geochemistry, geophysics, geosystems 14 (2013). doi:10.1002/2013GC004946
info:cnr-pdr/source/autori:Giulio Speranza, Domenico Cosentino, Francesca Tecce, Claudio Faccenna/titolo:Paleoclimate reconstruction during the Messinian evaporative drawdown of the Mediterranean Basin: Insights from microthermometry on halite fluid inclusions/doi:10.1002%2F2013GC004946/rivista:Geochemistry, geophysics, geosystems/anno:2013/pagina_da:/pagina_a:/intervallo_pagine:/volume:14

""Data constraining the paleoenvironmental conditions during the Messinian evaporative drawdown of the. Mediterranean basin are still conflicting. Here we present a comprehensive paleoclimatic reconstruction. during Messinian halite deposition from s

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::2acc9fd8802be1e7f262449d4ecc0800
https://hdl.handle.net/11590/135822

Fluid-rock interaction in an exhumed ductile-to-brittle shear zone: evidence for meteoric fluid infiltration at the depth of the brittle-ductile transition during the post-orogenic evolution of the Schistes Lustrés Nappe, Alpine Corsica (France

Autor: MAGGI, MATTEO, Rossetti, F., Simeone, N., Tecce, F., Vignaroli, G.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______3668::e105e96aa30d5dc15d0510bfdda5d2a2
https://hdl.handle.net/11590/187387