The Gavorrano Monzogranite (Northern Apennines): An Updated Review of Host Rock Protoliths, Thermal Metamorphism and Tectonic Setting

Autor: Brogi A.[1, Caggianelli A.[1], Liotta D.[1, Zucchi M.[1], Spina A.[3], Capezzuoli E.[4], Casini A.[5, Buracchi E.[5

Publikováno v: Geosciences
Volume 11
Issue 3
Geosciences, Vol 11, Iss 124, p 124 (2021)
Geosciences (Basel) 11 (2021): 1–30. doi:10.3390/geosciences11030124
info:cnr-pdr/source/autori:Brogi A.[1,2], Caggianelli A.[1], Liotta D.[1,2], Zucchi M.[1], Spina A.[3], Capezzuoli E.[4], Casini A.[5,6], Buracchi E.[5,6]/titolo:The Gavorrano Monzogranite (Northern Apennines): An Updated Review of Host Rock Protoliths, Thermal Metamorphism and Tectonic Setting./doi:10.3390%2Fgeosciences11030124/rivista:Geosciences (Basel)/anno:2021/pagina_da:1/pagina_a:30/intervallo_pagine:1–30/volume:11

We review and refine the geological setting of an area located nearby the Tyrrhenian seacoast, in the inner zone of the Northern Apennines (southern Tuscany), where a Neogene monzogranite body (estimated in about 3 km long, 1.5 km wide, and 0.7 km th

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Analogue Geothermal Systems In Mexico: Insights Into The Deep Part Of Los Humeros Geothermal Field From The Las Minas Mining Area (Eastern Mexico)

Autor: Liotta D.[1], Bastesen E.[2], Bianco C.[1], Brogi A.[1], Caggianelli A.[1], Garduño-Monroy V.H.[3], Gonzalez-Partida E.[4], Jimenez-Haro A.[3], Kozdrój W.[5], Lacinska A.[6], Lepillier B.[7], Morelli G.[8], Nawrocki J.[5], Olvera-Garcia E.[1], Panczyk-Nawrocka M.[5], Rochelle C.[6], Ruggieri G.[8], Torabi A.[2], Ventruti G.[1], Wheeler H.W.[2], Wójcik K.[5], Zió?kowska-Kozdrój M.[5], Zucchi M.[1]

Publikováno v: World Geothermal Congress (WGC) 2020+1, pp. 1–9, Reykjavik, Iceland, April-October 2021
info:cnr-pdr/source/autori:Liotta D.[1], Bastesen E.[2], Bianco C.[1], Brogi A.[1], Caggianelli A.[1], Garduño-Monroy V.H.[3], Gonzalez-Partida E.[4], Jimenez-Haro A.[3], Kozdrój W.[5], Lacinska A.[6], Lepillier B.[7], Morelli G.[8], Nawrocki J.[5], Olvera-Garcia E.[1], Panczyk-Nawrocka M.[5], Rochelle C.[6], Ruggieri G.[8], Torabi A.[2], Ventruti G.[1], Wheeler H.W.[2], Wójcik K.[5], Zió?kowska-Kozdrój M.[5], Zucchi M.[1]/congresso_nome:World Geothermal Congress (WGC) 2020+1/congresso_luogo:Reykjavik, Iceland/congresso_data:April-October 2021/anno:2021/pagina_da:1/pagina_a:9/intervallo_pagine:1–9

This study is part of the H2020-GEMex Project, a collaboration between Europe and Mexico for investigating super-hot geothermal systems. The novelty of this work is in its integrated methodological approach which bridges the past to the present and c

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https://publications.cnr.it/doc/459228

Geological Assessment of Castelnuovo (Italy) Demonstration Site for CO2 Reinjection in Deep Geothermal Reservoir. H2020 GECO Project

Autor: Trumpy E.[1], Baneschi I.[1], Batini F.[2], Bicocchi G.[3], Bonini M.[3], Botteghi S.[1], Brogi A.[1], Dini A.[1], Gola G.[1], Jeannin L.[4], Lelli M.[1], Liotta D.[1], Norelli F.[1], Manzella A.[1], Montanari D.[3], Montegrossi G.[3], Orlando A.[3], Raco B.[1], Ronconi A.[2], Ruggieri G.[3], Santilano A.[1], Souque C.[5], Boschi C.[1]

Publikováno v: World Geothermal Congress (WGC) 2020+1, pp. 1–11, Reykjavik, Iceland, April-October 2021
info:cnr-pdr/source/autori:Trumpy E.[1], Baneschi I.[1], Batini F.[2], Bicocchi G.[3], Bonini M.[3], Botteghi S.[1], Brogi A.[1], Dini A.[1], Gola G.[1], Jeannin L.[4], Lelli M.[1], Liotta D.[1], Norelli F.[1], Manzella A.[1], Montanari D.[3], Montegrossi G.[3], Orlando A.[3], Raco B.[1], Ronconi A.[2], Ruggieri G.[3], Santilano A.[1], Souque C.[5], Boschi C.[1]/congresso_nome:World Geothermal Congress (WGC) 2020+1/congresso_luogo:Reykjavik, Iceland/congresso_data:April-October 2021/anno:2021/pagina_da:1/pagina_a:11/intervallo_pagine:1–11

The EU H2020 GECO project is primarily aimed to set-up technologies to lower emissions from geothermal power generation by capturing them for either reuse or storage, to turn captured emissions in to commercial products and demonstrate the technical

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::d1ba1c1d9bca503daf741e1ed7f43ed9
https://publications.cnr.it/doc/459247

Permeability and hydraulic conductivity of faulted micaschist in the eastern Elba Island exhumed geothermal system (Tyrrhenian sea, Italy): insights from Cala Stagnone

Autor: Zucchi M.[1], Brogi A.[1], Liotta D.[1, Rimondi V.[2], Ruggieri G.[2], Montegrossi G.[2], Caggianelli A.[1], Dini A. [3]

Publikováno v: Geothermics 70 (2017): 125–145. doi:10.1016/j.geothermics.2017.05.007
info:cnr-pdr/source/autori:Zucchi M.[1], Brogi A.[1], Liotta D.[1,3], Rimondi V.[2], Ruggieri G.[2], Montegrossi G.[2], Caggianelli A.[1], Dini A. [3]/titolo:Permeability and hydraulic conductivity of faulted micaschist in the eastern Elba Island exhumed geothermal system (Tyrrhenian sea, Italy): insights from Cala Stagnone/doi:10.1016%2Fj.geothermics.2017.05.007/rivista:Geothermics/anno:2017/pagina_da:125/pagina_a:145/intervallo_pagine:125–145/volume:70

Estimating values of permeability (k), efficient porosity (P) and hydraulic conductivity (K) by analysing field outcrops as analogue of geothermal reservoirs, is a timely theme useful for predictions during geothermal exploration programs. In this pa

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a1644734db8445335ae6a09fa183b6d9
https://doi.org/10.1016/j.geothermics.2017.05.007

Field evidence of the interplay between rift and transform structures in the Krafla geothermal area, N-Iceland

Autor: Liotta D.[1, Brogi A.[1, Arnadottir S.[3], Thorsteinsdottir U. [3]

Publikováno v: Geothermics 91 (2021): 1–15. doi:10.1016/j.geothermics.2020.102039
info:cnr-pdr/source/autori:Liotta D.[1,2], Brogi A.[1,2], Arnadottir S.[3], Thorsteinsdottir U. [3]/titolo:Field evidence of the interplay between rift and transform structures in the Krafla geothermal area, N-Iceland/doi:10.1016%2Fj.geothermics.2020.102039/rivista:Geothermics/anno:2021/pagina_da:1/pagina_a:15/intervallo_pagine:1–15/volume:91

The Krafla volcano-geothermal area is located in Northeast Iceland, within the active Northern Volcanic Zone sector of the axial rift and has experienced two eruptions in historical times. The Krafla system displays NNE-SSW oriented fissure swarm, a

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b1c8423e069ce9d253e8c8bc2ec9a6b9
https://doi.org/10.1016/j.geothermics.2020.102039