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

Sulfide deposits from south-eastern Tyrrhenian Sea: new geochemical, isotopic and fluid inclusion data

Autor: Dini A. (1), Boschi C. (1), Gamberi F. (2), Laurenzi MA. (1), Marani M. (2), Rovere M. (2), Ruggieri G. (3), Trua T. (4)

Publikováno v: Rendiconti online Società Geologica Italiana 31 (2014): 18–18. doi:10.3301/ROL.2014.140
info:cnr-pdr/source/autori:Dini A. (1), Boschi C. (1), Gamberi F. (2), Laurenzi MA. (1), Marani M. (2), Rovere M. (2), Ruggieri G. (3), Trua T. (4)/titolo:Sulfide deposits from south-eastern Tyrrhenian Sea: new geochemical, isotopic and fluid inclusion data/doi:10.3301%2FROL.2014.140/rivista:Rendiconti online Società Geologica Italiana/anno:2014/pagina_da:18/pagina_a:18/intervallo_pagine:18–18/volume:31

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::b2c87da561bb087c357c5c06d2ca5ff2
https://publications.cnr.it/doc/319397

Direct carbon dioxide uptake from the atmosphere: examples from Montecastelli serpentinites (Tuscany, Italy)

Autor: Boschi C. [1], Dini A. [1], Baneschi I. [1], Bedini F. [1, Dallai L. [1], Perchiazzi N. [2]

Publikováno v: Proceeding of the 4th International Conference on accelerated carbonation for environmental and materials engineering. (ACEME 2013)., edited by Rabab N., Santos R., Cizer Ö., Van Gerven T (eds.)., pp. 431–441, 2013
info:cnr-pdr/source/autori:Boschi C. [1], Dini A. [1], Baneschi I. [1], Bedini F. [1, 2], Dallai L. [1], Perchiazzi N. [2]/titolo:Direct carbon dioxide uptake from the atmosphere: examples from Montecastelli serpentinites (Tuscany, Italy)/titolo_volume:Proceeding of the 4th International Conference on accelerated carbonation for environmental and materials engineering. (ACEME 2013)./curatori_volume:Rabab N., Santos R., Cizer Ö., Van Gerven T (eds.)./editore:/anno:2013

Atmospheric CO2 is spontaneously sequestered through the carbonation of serpentinites at Montecastelli (Tuscany, Italy). In the studied area, hydrated Mg-carbonates frequently form crusts, coating and spherules on exposed surfaces, in rock fractures,

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::0606a49c5ab3db938ed7093964db39b4
https://publications.cnr.it/doc/265303

Influence of seawater circulation on the evolution of ultramafic spreading ridges

Autor: Boschi, C.(1), Dini, A. (1), Frueh-Green, G. (2)

Publikováno v: Marine Research at CNR, edited by Brugnoli E., Cavarretta G., Mazzola S., Trincardi F., Ravaioli M., Santoleri R. (eds), pp. 399–408, 2011
info:cnr-pdr/source/autori:Boschi, C.(1); Dini, A. (1); Frueh-Green, G. (2)/titolo:Influence of seawater circulation on the evolution of ultramafic spreading ridges/titolo_volume:Marine Research at CNR/curatori_volume:Brugnoli E., Cavarretta G., Mazzola S., Trincardi F., Ravaioli M., Santoleri R. (eds)/editore:/anno:2011

A mid-oceanic ridge is an underwater mountain range formed by the diverging motion of tectonic plates that triggers the production of new lithosphere and the spreading of seafloor. The mid-ocean ridges of the world are connected and form a single glo

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::3adf91d761425f1fa55e1146bd4eae2b
https://publications.cnr.it/doc/203042

Levigliani e Ripa. Storia, genesi e mineralogia dei giacimenti mercuriferi

Autor: Dini A. (1), Biagioni C. (2)

Publikováno v: Rivista mineralogica italiana 34 (2010): 12–35.
info:cnr-pdr/source/autori:Dini A. (1); Biagioni C. (2)/titolo:Levigliani e Ripa. Storia, genesi e mineralogia dei giacimenti mercuriferi./doi:/rivista:Rivista mineralogica italiana/anno:2010/pagina_da:12/pagina_a:35/intervallo_pagine:12–35/volume:34

Le piccole miniere di mercurio di Levigliani e Ripa nelle Alpi Apuane (Toscana), coltivate in modo discontinuo dal Medioevo fino al 1970, non hanno avuto un rilievo industriale paragonabile a quelle del Monte Amiata, ma sono conosciute nell'ambiente

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::291a47b6ce8764830a2294ee594a6007
http://www.cnr.it/prodotto/i/64000