Zobrazeno 1 - 10
of 94
pro vyhledávání: '"G. 6"'
Publikováno v:
Journal of Maps
Journal of Maps, Taylor & Francis, 2021, 17 (2), pp.559-568. ⟨10.1080/17445647.2021.1982034⟩
Journal of Maps, 2021, 17 (2), pp.559-568. ⟨10.1080/17445647.2021.1982034⟩
Journal of maps 17 (2021): 559–568. doi:10.1080/17445647.2021.1982034
info:cnr-pdr/source/autori:Sanità E.[1,2], Lardeaux J.-M.[3,4], Marroni M.[1,5], Gosso G.[6], Pandolfi L.[1,5]/titolo:Deciphering large-scale superposed fold systems at shallow crustal levels in collision zones: insights from the Marguareis Massif (southwestern Alps)/doi:10.1080%2F17445647.2021.1982034/rivista:Journal of maps/anno:2021/pagina_da:559/pagina_a:568/intervallo_pagine:559–568/volume:17
Journal of Maps, Vol 17, Iss 2, Pp 571-580 (2021)
Journal of Maps, Taylor & Francis, 2021, 17 (2), pp.559-568. ⟨10.1080/17445647.2021.1982034⟩
Journal of Maps, 2021, 17 (2), pp.559-568. ⟨10.1080/17445647.2021.1982034⟩
Journal of maps 17 (2021): 559–568. doi:10.1080/17445647.2021.1982034
info:cnr-pdr/source/autori:Sanità E.[1,2], Lardeaux J.-M.[3,4], Marroni M.[1,5], Gosso G.[6], Pandolfi L.[1,5]/titolo:Deciphering large-scale superposed fold systems at shallow crustal levels in collision zones: insights from the Marguareis Massif (southwestern Alps)/doi:10.1080%2F17445647.2021.1982034/rivista:Journal of maps/anno:2021/pagina_da:559/pagina_a:568/intervallo_pagine:559–568/volume:17
Journal of Maps, Vol 17, Iss 2, Pp 571-580 (2021)
International audience; We present and discuss the results of a field-based approach including accurate geological mapping and micro-to map-scale structural analysis to highlight the finite strain pattern recorded in Marguareis Unit, a massif deforme
Autor:
Russo Ermolli E.[1], Masi A.[2, Vignola C.[2], Di Lorenzo H.[1], Masci L.[2], Bona F.[4], Forti L.[4, Lembo G.[6], Mazzini I.[7], Mecozzi B.[8], Muttillo B.[6], Pieruccini P.[9], Sardella R.[8], Sadori L.[2]
Publikováno v:
Review of palaeobotany and palynology 297 (2022). doi:10.1016/j.revpalbo.2021.104577
info:cnr-pdr/source/autori:Russo Ermolli E.[1], Masi A.[2,3], Vignola C.[2], Di Lorenzo H.[1], Masci L.[2], Bona F.[4], Forti L.[4,5], Lembo G.[6], Mazzini I.[7], Mecozzi B.[8], Muttillo B.[6], Pieruccini P.[9], Sardella R.[8], Sadori L.[2]/titolo:The pollen record from Grotta Romanelli (Apulia, Italy): New insight for the Late Pleistocene Mediterranean vegetation and plant use/doi:10.1016%2Fj.revpalbo.2021.104577/rivista:Review of palaeobotany and palynology/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:297
info:cnr-pdr/source/autori:Russo Ermolli E.[1], Masi A.[2,3], Vignola C.[2], Di Lorenzo H.[1], Masci L.[2], Bona F.[4], Forti L.[4,5], Lembo G.[6], Mazzini I.[7], Mecozzi B.[8], Muttillo B.[6], Pieruccini P.[9], Sardella R.[8], Sadori L.[2]/titolo:The pollen record from Grotta Romanelli (Apulia, Italy): New insight for the Late Pleistocene Mediterranean vegetation and plant use/doi:10.1016%2Fj.revpalbo.2021.104577/rivista:Review of palaeobotany and palynology/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:297
Pollen analyses have been carried out on the infilling deposits of Grotta Romanelli (Apulia, Italy), a reference site for the Middle and Upper Palaeolithic of Italy. The analysis focused on Terre rosse, a fine unit till now ascribed to an interstadia
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8fc671bec531855e2afc8d98dc0b060a
https://hdl.handle.net/11365/1223782
https://hdl.handle.net/11365/1223782
Autor:
Giaccherini A.[1, 2, Cucinotta G.[4], Martinuzzi S.[4], Berretti E.[5], Oberhauser W.[5], Lavacchi A.[5], Lepore G.[6], Montegrossi G.[7], Romanelli M.[1], De Luca A.[4], Innocenti M.[3, 4, Moggi Cecchi V.[8], Mannini M.[3, Buccianti A.[1], Di Benedetto F.[1]
Publikováno v:
Beilstein Journal of Nanotechnology, Vol 10, Iss 1, Pp 2073-2083 (2019)
Beilstein journal of nanotechnology 10 (2019): 2073–2083. doi:10.3762/bjnano.10.202
info:cnr-pdr/source/autori:Giaccherini A.[1,2,3], Cucinotta G.[4], Martinuzzi S.[4], Berretti E.[5], Oberhauser W.[5], Lavacchi A.[5], Lepore G.[6], Montegrossi G.[7], Romanelli M.[1], De Luca A.[4], Innocenti M.[3,4,5], Moggi Cecchi V.[8], Mannini M.[3,4], Buccianti A.[1], Di Benedetto F.[1]/titolo:Green and scalable synthesis of nanocrystalline kuramite/doi:10.3762%2Fbjnano.10.202/rivista:Beilstein journal of nanotechnology/anno:2019/pagina_da:2073/pagina_a:2083/intervallo_pagine:2073–2083/volume:10
Beilstein Journal of Nanotechnology
Beilstein journal of nanotechnology 10 (2019): 2073–2083. doi:10.3762/bjnano.10.202
info:cnr-pdr/source/autori:Giaccherini A.[1,2,3], Cucinotta G.[4], Martinuzzi S.[4], Berretti E.[5], Oberhauser W.[5], Lavacchi A.[5], Lepore G.[6], Montegrossi G.[7], Romanelli M.[1], De Luca A.[4], Innocenti M.[3,4,5], Moggi Cecchi V.[8], Mannini M.[3,4], Buccianti A.[1], Di Benedetto F.[1]/titolo:Green and scalable synthesis of nanocrystalline kuramite/doi:10.3762%2Fbjnano.10.202/rivista:Beilstein journal of nanotechnology/anno:2019/pagina_da:2073/pagina_a:2083/intervallo_pagine:2073–2083/volume:10
Beilstein Journal of Nanotechnology
The new generation of solar cells aims to overcome many of the issues created by silicon-based devices (e.g., decommissioning, flexibility and high-energy production costs). Due to the scarcity of the resources involved in the process and the need fo
Autor:
Calcagno P.[1], Trumpy E.[2], Gutiérrez-Negrín L.C.[3], Norini G.[4], Macías J.L.[5], Carrasco-Núñez G.[6], Liotta D.[7], Garduño-Monroy V.H.[8], Hersir G.P.[9], Vaessen L.[10], Evanno G.[1, Arango Galván C.[11]
Publikováno v:
World Geothermal Congress (WGC) 2020+1, pp. 1–12, Reykjavik, Iceland, April-October 2021
info:cnr-pdr/source/autori:Calcagno P.[1], Trumpy E.[2], Gutiérrez-Negrín L.C.[3], Norini G.[4], Macías J.L.[5], Carrasco-Núñez G.[6], Liotta D.[7], Garduño-Monroy V.H.[8], Hersir G.P.[9], Vaessen L.[10], Evanno G.[1,#], Arango Galván C.[11]/congresso_nome:World Geothermal Congress (WGC) 2020+1/congresso_luogo:Reykjavik, Iceland/congresso_data:April-October 2021/anno:2021/pagina_da:1/pagina_a:12/intervallo_pagine:1–12
info:cnr-pdr/source/autori:Calcagno P.[1], Trumpy E.[2], Gutiérrez-Negrín L.C.[3], Norini G.[4], Macías J.L.[5], Carrasco-Núñez G.[6], Liotta D.[7], Garduño-Monroy V.H.[8], Hersir G.P.[9], Vaessen L.[10], Evanno G.[1,#], Arango Galván C.[11]/congresso_nome:World Geothermal Congress (WGC) 2020+1/congresso_luogo:Reykjavik, Iceland/congresso_data:April-October 2021/anno:2021/pagina_da:1/pagina_a:12/intervallo_pagine:1–12
he European-Mexican geothermal GEMex project aims at developing geothermal energy in the easternmost region of the TransMexican Volcanic Belt. Two sites under development by the Comisión Federal de Electricidad (Mexican National Power Company) are i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::2dc672112e4dabc61b1b966cea25a9e2
https://publications.cnr.it/doc/459217
https://publications.cnr.it/doc/459217
Autor:
Brombin V.[1], Bonadiman C.[1], Jourdan F.[2], Roghi G.[3], Coltorti M.[1], Webb L.E.[4], Callegaro S.[5], Bellieni G.[6], De Vecchi G.[6], Sede R.[1, Marzoli A.[3
Publikováno v:
Earth-science reviews 192 (2019): 355–378. doi:10.1016/j.earscirev.2019.03.016
info:cnr-pdr/source/autori:Brombin V.[1], Bonadiman C.[1], Jourdan F.[2], Roghi G.[3], Coltorti M.[1], Webb L.E.[4], Callegaro S.[5], Bellieni G.[6], De Vecchi G.[6], Sede R.[1,6], Marzoli A.[3,6]/titolo:Intraplate magmatism at a convergent plate boundary: The case of the Cenozoic northern Adria magmatism/doi:10.1016%2Fj.earscirev.2019.03.016/rivista:Earth-science reviews/anno:2019/pagina_da:355/pagina_a:378/intervallo_pagine:355–378/volume:192
info:cnr-pdr/source/autori:Brombin V.[1], Bonadiman C.[1], Jourdan F.[2], Roghi G.[3], Coltorti M.[1], Webb L.E.[4], Callegaro S.[5], Bellieni G.[6], De Vecchi G.[6], Sede R.[1,6], Marzoli A.[3,6]/titolo:Intraplate magmatism at a convergent plate boundary: The case of the Cenozoic northern Adria magmatism/doi:10.1016%2Fj.earscirev.2019.03.016/rivista:Earth-science reviews/anno:2019/pagina_da:355/pagina_a:378/intervallo_pagine:355–378/volume:192
The complex European–Adria geodynamic framework, which led to the formation of the Alpine belt, is considered responsible for the orogenic magmatism that occurred in the Central Alps along the Periadriatic/Insubric Line (late Eocene–early Oligoce
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a6be5f0574f40f5fff99414592a1c027
https://publications.cnr.it/doc/463572
https://publications.cnr.it/doc/463572
Publikováno v:
Journal of Volcanology and Geothermal Research
Journal of Volcanology and Geothermal Research, 2018, 362, pp.64-75. ⟨10.1016/j.jvolgeores.2018.08.008⟩
Journal of volcanology and geothermal research 362 (2018): 64–75. doi:10.1016/j.jvolgeores.2018.08.008
info:cnr-pdr/source/autori:De Matteo A.[1], Corti G.[2,3], Van Wyk De Vries B.[4], Massa B.[1,5], Mussetti G. [6]/titolo:Fault-volcano interactions with broadly distributed stretching in rifts/doi:10.1016%2Fj.jvolgeores.2018.08.008/rivista:Journal of volcanology and geothermal research/anno:2018/pagina_da:64/pagina_a:75/intervallo_pagine:64–75/volume:362
Journal of Volcanology and Geothermal Research, 2018, 362, pp.64-75. ⟨10.1016/j.jvolgeores.2018.08.008⟩
Journal of volcanology and geothermal research 362 (2018): 64–75. doi:10.1016/j.jvolgeores.2018.08.008
info:cnr-pdr/source/autori:De Matteo A.[1], Corti G.[2,3], Van Wyk De Vries B.[4], Massa B.[1,5], Mussetti G. [6]/titolo:Fault-volcano interactions with broadly distributed stretching in rifts/doi:10.1016%2Fj.jvolgeores.2018.08.008/rivista:Journal of volcanology and geothermal research/anno:2018/pagina_da:64/pagina_a:75/intervallo_pagine:64–75/volume:362
Areas undergoing pure extension are typically characterized by the formation of faults and fractures orthogonal to the maximum principal stress. In these conditions, the presence of a volcano and its magmatic system perturbs the local stress field, l
Autor:
Taussi M.[1], Godoy B.[2], Piscaglia F.[3], Morata D.[2], Agostini A.[4], Le Roux P.[5], González-Maurel O.[5, Gallmeyer G.[6], Menzies A.[6], Renzulli A.[1
Publikováno v:
Journal of volcanology and geothermal research 373 (2019): 179–198. doi:10.1016/j.jvolgeores.2019.01.021
info:cnr-pdr/source/autori:Taussi M.[1], Godoy B.[2], Piscaglia F.[3], Morata D.[2], Agostini A.[4], Le Roux P.[5], González-Maurel O.[5,6], Gallmeyer G.[6], Menzies A.[6], Renzulli A.[1,3]/titolo:The upper crustal magma plumbing system of the Pleistocene Apacheta-Aguilucho Volcanic Complex area (Altiplano-Puna, northern Chile) as inferred from the erupted lavas and their enclaves/doi:10.1016%2Fj.jvolgeores.2019.01.021/rivista:Journal of volcanology and geothermal research/anno:2019/pagina_da:179/pagina_a:198/intervallo_pagine:179–198/volume:373
info:cnr-pdr/source/autori:Taussi M.[1], Godoy B.[2], Piscaglia F.[3], Morata D.[2], Agostini A.[4], Le Roux P.[5], González-Maurel O.[5,6], Gallmeyer G.[6], Menzies A.[6], Renzulli A.[1,3]/titolo:The upper crustal magma plumbing system of the Pleistocene Apacheta-Aguilucho Volcanic Complex area (Altiplano-Puna, northern Chile) as inferred from the erupted lavas and their enclaves/doi:10.1016%2Fj.jvolgeores.2019.01.021/rivista:Journal of volcanology and geothermal research/anno:2019/pagina_da:179/pagina_a:198/intervallo_pagine:179–198/volume:373
The evolution of the magma plumbing system of the Pleistocene Apacheta-Aguilucho Volcanic Complex area (Altiplano-Puna Volcanic Complex, northern Chile) was investigated through petrographic, geochemical and isotopic studies of representative lavas a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::182ba00063760c305b4e7c49b0043bea
https://hdl.handle.net/11576/2665116
https://hdl.handle.net/11576/2665116
Autor:
Taussi M.[1], Nisi B.[2], Pizarro M.[3, Morata D.[3, Veloso E.A.[4, Volpi G.[6] Vaselli O.[2, 7] Renzulli A.[1]
Publikováno v:
Journal of volcanology and geothermal research 384 (2019): 1–14. doi:10.1016/j.jvolgeores.2019.07.009
info:cnr-pdr/source/autori:Taussi M.[1], Nisi B.[2], Pizarro M.[3,4], Morata D.[3,4], Veloso E.A.[4,5], Volpi G.[6] Vaselli O.[2,7] Renzulli A.[1]/titolo:Sealing capacity of clay-cap units above the Cerro Pabellón hidden geothermal system (northern Chile) derived by soil CO2 flux and temperature measurements/doi:10.1016%2Fj.jvolgeores.2019.07.009/rivista:Journal of volcanology and geothermal research/anno:2019/pagina_da:1/pagina_a:14/intervallo_pagine:1–14/volume:384
info:cnr-pdr/source/autori:Taussi M.[1], Nisi B.[2], Pizarro M.[3,4], Morata D.[3,4], Veloso E.A.[4,5], Volpi G.[6] Vaselli O.[2,7] Renzulli A.[1]/titolo:Sealing capacity of clay-cap units above the Cerro Pabellón hidden geothermal system (northern Chile) derived by soil CO2 flux and temperature measurements/doi:10.1016%2Fj.jvolgeores.2019.07.009/rivista:Journal of volcanology and geothermal research/anno:2019/pagina_da:1/pagina_a:14/intervallo_pagine:1–14/volume:384
Cerro Pabellon is a hidden high-enthalpy geothermal system (reservoir temperature up to 250 °C) located in the Pampa Apacheta (northern Chile), where the first geothermal power plant in South America is currently operating. A fumarolic field, locate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7efd34a4f74bb21bf031c2f09a7bda6e
http://www.cnr.it/prodotto/i/409155
http://www.cnr.it/prodotto/i/409155
Autor:
Chiodi A.[1], Tassi F.[2, Baéz W.[1], Filipovich R.[1], Bustos E.[1], Glok Galli M.[4], Suzaño N.[5], Ahumada M.F.[1], Viramonte J.[1], Giordano G.[6, Pecoraino G.[8], Vaselli O.[2
Publikováno v:
Journal of South American earth sciences 94 (2019).
info:cnr-pdr/source/autori:Chiodi A.[1], Tassi F.[2,3], Baéz W.[1], Filipovich R.[1], Bustos E.[1], Glok Galli M.[4], Suzaño N.[5], Ahumada M.F.[1], Viramonte J.[1], Giordano G.[6,7], Pecoraino G.[8], Vaselli O.[2,3]/titolo:Preliminary conceptual model of the Cerro Bianco caldera-hosted geothermal system (Southern Puna, Argentina): Inferences from geochemical investigations/doi:/rivista:Journal of South American earth sciences/anno:2019/pagina_da:/pagina_a:/intervallo_pagine:/volume:94
info:cnr-pdr/source/autori:Chiodi A.[1], Tassi F.[2,3], Baéz W.[1], Filipovich R.[1], Bustos E.[1], Glok Galli M.[4], Suzaño N.[5], Ahumada M.F.[1], Viramonte J.[1], Giordano G.[6,7], Pecoraino G.[8], Vaselli O.[2,3]/titolo:Preliminary conceptual model of the Cerro Bianco caldera-hosted geothermal system (Southern Puna, Argentina): Inferences from geochemical investigations/doi:/rivista:Journal of South American earth sciences/anno:2019/pagina_da:/pagina_a:/intervallo_pagine:/volume:94
Not available
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::68826c1d7e561ebbf74b611fae6d6f62
https://publications.cnr.it/doc/407360
https://publications.cnr.it/doc/407360