Zobrazeno 1 - 10
of 11
pro vyhledávání: '"Conticelli S. [1"'
Autor:
Casalini M.[1], Tommasini S.[1], Guarnieri L.[1], Avanzinelli R.[1, Lanari R.[1], Mattei M.[3], Conticelli S.[1
Publikováno v:
Italian Journal of Geosciences (Testo stamp.) 141 (2022): 144–159. doi:10.3301/IJG.2022.06
info:cnr-pdr/source/autori:Casalini M.[1], Tommasini S.[1], Guarnieri L.[1], Avanzinelli R.[1,2], Lanari R.[1], Mattei M.[3], Conticelli S.[1,4]/titolo:Subduction-related lamproitic signature in intraplate-like volcanic rocks: the case study of the Tallante alkali basalts, Betic Chain, South-Eastern Spain/doi:10.3301%2FIJG.2022.06/rivista:Italian Journal of Geosciences (Testo stamp.)/anno:2022/pagina_da:144/pagina_a:159/intervallo_pagine:144–159/volume:141
info:cnr-pdr/source/autori:Casalini M.[1], Tommasini S.[1], Guarnieri L.[1], Avanzinelli R.[1,2], Lanari R.[1], Mattei M.[3], Conticelli S.[1,4]/titolo:Subduction-related lamproitic signature in intraplate-like volcanic rocks: the case study of the Tallante alkali basalts, Betic Chain, South-Eastern Spain/doi:10.3301%2FIJG.2022.06/rivista:Italian Journal of Geosciences (Testo stamp.)/anno:2022/pagina_da:144/pagina_a:159/intervallo_pagine:144–159/volume:141
South-Eastern Spain is a key locality of the Western Mediterranean to unravel the origin of post-collisional magmatism and its relationships with the multi-stage evolution of the upper mantle in complex geodynamic settings. This study is focused on t
Autor:
Casalini M.[1], Avanzinelli R.[1, Tommasini S.[1], Natali C.[1, Bianchini G.[4], Prelevic? D.[5, Mattei M.[7], Conticelli S.[1
Publikováno v:
Special publication-Geological Society of London 513 (2022): 271–296. doi:10.1144/SP513-2021-36
info:cnr-pdr/source/autori:Casalini M.[1], Avanzinelli R.[1,2], Tommasini S.[1], Natali C.[1,3], Bianchini G.[4], Prelevic? D.[5,6], Mattei M.[7], Conticelli S.[1,3]/titolo:Petrogenesis of Mediterranean lamproites and associated rocks: The role of overprinted metasomatic events in the post-collisional lithospheric upper mantle/doi:10.1144%2FSP513-2021-36/rivista:Special publication-Geological Society of London/anno:2022/pagina_da:271/pagina_a:296/intervallo_pagine:271–296/volume:513
info:cnr-pdr/source/autori:Casalini M.[1], Avanzinelli R.[1,2], Tommasini S.[1], Natali C.[1,3], Bianchini G.[4], Prelevic? D.[5,6], Mattei M.[7], Conticelli S.[1,3]/titolo:Petrogenesis of Mediterranean lamproites and associated rocks: The role of overprinted metasomatic events in the post-collisional lithospheric upper mantle/doi:10.1144%2FSP513-2021-36/rivista:Special publication-Geological Society of London/anno:2022/pagina_da:271/pagina_a:296/intervallo_pagine:271–296/volume:513
High-MgO lamproite and lamproite-like (i.e. lamprophyric) ultrapotassic rocks are recurrent in the Mediterranean and surrounding regions. They are associated in space and time with ultrapotassic shoshonites and high-K calc-alkaline rocks. This magmat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b7850dfa95b78313a9b41492e0ba7486
Autor:
Avanzinelli R.[1, Bianchini G.[3], Tiepolo M.[4], Jasim A.[1, Natali C.[1], Braschi E.[2], Dallai L.[6], Beccaluva L.[3], Conticelli S.[1
Publikováno v:
Lithos (Oslo. Print) 352-353 (2020): 1–17. doi:10.1016/j.lithos.2019.105316
info:cnr-pdr/source/autori:Avanzinelli R.[1,2], Bianchini G.[3], Tiepolo M.[4], Jasim A.[1,5], Natali C.[1], Braschi E.[2], Dallai L.[6], Beccaluva L.[3], Conticelli S.[1,7]/titolo:Subduction-related hybridization of the lithospheric mantle revealed by trace element and Sr-Nd-Pb isotopic data in composite xenoliths from Tallante (Betic Cordillera, Spain)/doi:10.1016%2Fj.lithos.2019.105316/rivista:Lithos (Oslo. Print)/anno:2020/pagina_da:1/pagina_a:17/intervallo_pagine:1–17/volume:352-353
info:cnr-pdr/source/autori:Avanzinelli R.[1,2], Bianchini G.[3], Tiepolo M.[4], Jasim A.[1,5], Natali C.[1], Braschi E.[2], Dallai L.[6], Beccaluva L.[3], Conticelli S.[1,7]/titolo:Subduction-related hybridization of the lithospheric mantle revealed by trace element and Sr-Nd-Pb isotopic data in composite xenoliths from Tallante (Betic Cordillera, Spain)/doi:10.1016%2Fj.lithos.2019.105316/rivista:Lithos (Oslo. Print)/anno:2020/pagina_da:1/pagina_a:17/intervallo_pagine:1–17/volume:352-353
Ultramafic xenoliths are rarely found at convergent plate margins. A notable exception is in the Betic Cordillera of southern Spain, where the eruption of xenolith-bearing alkaline basalts during the Pliocene post-dated the Cenozoic phase of plate co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8dcf219ec43ec245bbe2a1aa6aea2581
http://hdl.handle.net/2158/1192267
http://hdl.handle.net/2158/1192267
Autor:
Braschi E.[1, Marchionni S.[3, Priori S.[2], Casalini M.[3], Tommasini S.[3], Natarelli L.[2], Buccianti A.[3], Bucelli P.[2], Costantini E.A.C.[2], Conticelli S.[1
Publikováno v:
Science of the total environment 628-629 (2018): 1317–1327. doi:10.1016/j.scitotenv.2018.02.069
info:cnr-pdr/source/autori:Braschi E.[1,2], Marchionni S.[3,4], Priori S.[2], Casalini M.[3], Tommasini S.[3], Natarelli L.[2], Buccianti A.[3], Bucelli P.[2], Costantini E.A.C.[2], Conticelli S.[1,3]/titolo:Tracing the Sr-87%2FSr-86 from rocks and soils to vine and wine: An experimental study on geologic and pedologic characterisation of vineyards using radiogenic isotope of heavy elements/doi:10.1016%2Fj.scitotenv.2018.02.069/rivista:Science of the total environment/anno:2018/pagina_da:1317/pagina_a:1327/intervallo_pagine:1317–1327/volume:628-629
info:cnr-pdr/source/autori:Braschi E.[1,2], Marchionni S.[3,4], Priori S.[2], Casalini M.[3], Tommasini S.[3], Natarelli L.[2], Buccianti A.[3], Bucelli P.[2], Costantini E.A.C.[2], Conticelli S.[1,3]/titolo:Tracing the Sr-87%2FSr-86 from rocks and soils to vine and wine: An experimental study on geologic and pedologic characterisation of vineyards using radiogenic isotope of heavy elements/doi:10.1016%2Fj.scitotenv.2018.02.069/rivista:Science of the total environment/anno:2018/pagina_da:1317/pagina_a:1327/intervallo_pagine:1317–1327/volume:628-629
In this paper we report an experimental study to assess the process of Sr-isotope uptake from the soil and its transfer to the grapevine and then to the wine made through micro-vinification. The experimental work has been carried out with a deep cont
Autor:
Di Salvo S.[1], Braschi E.[2], Casalini M.[1], Marchionni S.[1], Adani T.[1], Ulivi M.[1], Orlando A.[2], Tommasini S.[1], Avanzinelli R.[1, Mazza P.P.A.[1], Conticelli S.[1, Francalanci L.[1
Publikováno v:
Journal of Analytical Methods in Chemistry, Vol 2018 (2018)
Journal of Analytical Methods in Chemistry
Journal of Analytical Methods in Chemistry 2018 (2018): 1–20. doi:10.1155/2018/1292954
info:cnr-pdr/source/autori:Di Salvo S.[1], Braschi E.[2], Casalini M.[1], Marchionni S.[1], Adani T.[1], Ulivi M.[1], Orlando A.[2], Tommasini S.[1], Avanzinelli R.[1,2], Mazza P.P.A.[1], Conticelli S.[1,2], Francalanci L.[1,2]/titolo:High-Precision in Situ 87<%2Fsup>Sr%2F86<%2Fsup>Sr Analyses through Microsampling on Solid Samples: Applications to Earth and Life Sciences/doi:10.1155%2F2018%2F1292954/rivista:Journal of Analytical Methods in Chemistry/anno:2018/pagina_da:1/pagina_a:20/intervallo_pagine:1–20/volume:2018
Journal of Analytical Methods in Chemistry
Journal of Analytical Methods in Chemistry 2018 (2018): 1–20. doi:10.1155/2018/1292954
info:cnr-pdr/source/autori:Di Salvo S.[1], Braschi E.[2], Casalini M.[1], Marchionni S.[1], Adani T.[1], Ulivi M.[1], Orlando A.[2], Tommasini S.[1], Avanzinelli R.[1,2], Mazza P.P.A.[1], Conticelli S.[1,2], Francalanci L.[1,2]/titolo:High-Precision in Situ 87<%2Fsup>Sr%2F86<%2Fsup>Sr Analyses through Microsampling on Solid Samples: Applications to Earth and Life Sciences/doi:10.1155%2F2018%2F1292954/rivista:Journal of Analytical Methods in Chemistry/anno:2018/pagina_da:1/pagina_a:20/intervallo_pagine:1–20/volume:2018
An analytical protocol for high-precision, in situ microscale isotopic investigations is presented here, which combines the use of a high-performing mechanical microsampling device and high-precision TIMS measurements on micro-Sr samples, allowing fo
Autor:
Casalini M.[1], Pensa A.[2], Avanzinelli R.[1, Giordano G.[2], Mattei M.[2], Conticelli S.[1, 3
Publikováno v:
Memorie descrittive della carta geologica d'Italia 104 (2019): 9–30.
info:cnr-pdr/source/autori:Casalini M.[1], Pensa A.[2], Avanzinelli R.[1,3], Giordano G.[2], Mattei M.[2], Conticelli S.[1,3,4]/titolo:Geodynamics and magmatism of the Central Mediterranean region-Geodinamica e magmatismo della regione Centro-Mediterranea/doi:/rivista:Memorie descrittive della carta geologica d'Italia/anno:2019/pagina_da:9/pagina_a:30/intervallo_pagine:9–30/volume:104
info:cnr-pdr/source/autori:Casalini M.[1], Pensa A.[2], Avanzinelli R.[1,3], Giordano G.[2], Mattei M.[2], Conticelli S.[1,3,4]/titolo:Geodynamics and magmatism of the Central Mediterranean region-Geodinamica e magmatismo della regione Centro-Mediterranea/doi:/rivista:Memorie descrittive della carta geologica d'Italia/anno:2019/pagina_da:9/pagina_a:30/intervallo_pagine:9–30/volume:104
The Mediterranean area is one of the most intriguing places on Earth where geodynamics and volcanoes are strictly related, and evolved through time. The complexity of the tectonic setting is further enriched by the observed shift of the petrochemical
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::68f3f8da675695e5125c912c2c2e0069
http://www.cnr.it/prodotto/i/414476
http://www.cnr.it/prodotto/i/414476
Autor:
Casalini M.[1], Heumann A.[2], Marchionni S.[1], Conticelli S.[1, Avanzinelli R. [1, Tommasini S.[1]
Publikováno v:
Italian Journal of Geosciences (Online) 137 (2018): 420–432.
info:cnr-pdr/source/autori:Casalini M.[1], Heumann A.[2], Marchionni S.[1], Conticelli S.[1,3], Avanzinelli R. [1,3], Tommasini S.[1]/titolo:Inverse modelling to unravel the radiogenic isotope signature of mantle sources from envolved magmas: the case-study of Ischia volcano/doi:/rivista:Italian Journal of Geosciences (Online)/anno:2018/pagina_da:420/pagina_a:432/intervallo_pagine:420–432/volume:137
info:cnr-pdr/source/autori:Casalini M.[1], Heumann A.[2], Marchionni S.[1], Conticelli S.[1,3], Avanzinelli R. [1,3], Tommasini S.[1]/titolo:Inverse modelling to unravel the radiogenic isotope signature of mantle sources from envolved magmas: the case-study of Ischia volcano/doi:/rivista:Italian Journal of Geosciences (Online)/anno:2018/pagina_da:420/pagina_a:432/intervallo_pagine:420–432/volume:137
The active volcano of Ischia, the well-known island off-shore the city of Naples, has had a discontinuous volcanic activity characterised by caldera-forming paroxysmal eruptions, lava flows, and lava domes for >150 kyr. The overall geochemical compos
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::a2a03cbba4bce2895bd243111a31d200
https://publications.cnr.it/doc/392634
https://publications.cnr.it/doc/392634
Publikováno v:
Geology (Boulder Colo., Online) 46 (2018): 259–262. doi:10.1130/G39766.1
info:cnr-pdr/source/autori:Avanzinelli R.[1,2], Casalini M.[1], Elliott T.[2], Conticelli S.[1,3]/titolo:Carbon fluxes from subducted carbonates revealed by U excess at Vesuvius/doi:10.1130%2FG39766.1/rivista:Geology (Boulder Colo., Online)/anno:2018/pagina_da:259/pagina_a:262/intervallo_pagine:259–262/volume:46
info:cnr-pdr/source/autori:Avanzinelli R.[1,2], Casalini M.[1], Elliott T.[2], Conticelli S.[1,3]/titolo:Carbon fluxes from subducted carbonates revealed by U excess at Vesuvius/doi:10.1130%2FG39766.1/rivista:Geology (Boulder Colo., Online)/anno:2018/pagina_da:259/pagina_a:262/intervallo_pagine:259–262/volume:46
The fate of carbonate-rich sediments recycled at destructive plate margins is a key issue for constraining the budget of deep CO2 supplied to the atmosphere by volcanism. Experimental studies have demonstrated that metasomatic melts can be generated
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::aa1c553a730bb6201421f9954797458a
Autor:
Braschi E.[1, Marchionni S.[3, Priori S.[2], Casalini M.[3], Tommasini S.[3], Natarelli L.[2], Buccianti A.[3], Bucelli P.[2], Costantini E.A.C.[2], Conticelli S.[1
Publikováno v:
Data in brief 18 (2018): 731–735. doi:10.1016/j.scitotenv.2018.02.069
info:cnr-pdr/source/autori:Braschi E.[1,2], Marchionni S.[3,4], Priori S.[2], Casalini M.[3], Tommasini S.[3], Natarelli L.[2], Buccianti A.[3], Bucelli P.[2], Costantini E.A.C.[2], Conticelli S.[1,3]/titolo:From vine to wine: data on 87Sr%2F86Sr from rocks and soils as a geologic and pedologic characterisation of vineyards/doi:10.1016%2Fj.scitotenv.2018.02.069/rivista:Data in brief/anno:2018/pagina_da:731/pagina_a:735/intervallo_pagine:731–735/volume:18
info:cnr-pdr/source/autori:Braschi E.[1,2], Marchionni S.[3,4], Priori S.[2], Casalini M.[3], Tommasini S.[3], Natarelli L.[2], Buccianti A.[3], Bucelli P.[2], Costantini E.A.C.[2], Conticelli S.[1,3]/titolo:From vine to wine: data on 87Sr%2F86Sr from rocks and soils as a geologic and pedologic characterisation of vineyards/doi:10.1016%2Fj.scitotenv.2018.02.069/rivista:Data in brief/anno:2018/pagina_da:731/pagina_a:735/intervallo_pagine:731–735/volume:18
This data article describes the soils characterisation, bedrock geochemical composition and descriptive statistics of 87Sr/86Sr in wines, grape saps, labile fractions of soils (bio-available), whole soils, and bedrocks used to explore the Sr isotope
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::a02899bc6d2f3c3ce30ecd23e61672d5
https://www.journals.elsevier.com/data-in-brief
https://www.journals.elsevier.com/data-in-brief
Autor:
Conticelli S.[1], Boari E.[1], Burlamacchi L.[3], Cifelli F.[4], Moscardi F.[1], Laurenzi M.[5], Ferrari Pedraglio L.[6], Francalanci L.[1, Benvenuti M.[1, Braschi E., 2
Publikováno v:
Italian Journal of Geosciences (Online) 134 (2015): 266–290.
info:cnr-pdr/source/autori:Conticelli S.[1], Boari E.[1], Burlamacchi L.[3], Cifelli F.[4], Moscardi F.[1], Laurenzi M.[5], Ferrari Pedraglio L.[6], Francalanci L.[1,2], Benvenuti M.[1,2], Braschi E.,[2] Manetti P. [3]/titolo:Geochemistry and Sr-Nd-Pb isotopes of Monte Amiata volcano, central Italy: evidence for magma mixing between high-K calc-alkaline and leucititic mantle-derivd magmas/doi:/rivista:Italian Journal of Geosciences (Online)/anno:2015/pagina_da:266/pagina_a:290/intervallo_pagine:266–290/volume:134
info:cnr-pdr/source/autori:Conticelli S.[1], Boari E.[1], Burlamacchi L.[3], Cifelli F.[4], Moscardi F.[1], Laurenzi M.[5], Ferrari Pedraglio L.[6], Francalanci L.[1,2], Benvenuti M.[1,2], Braschi E.,[2] Manetti P. [3]/titolo:Geochemistry and Sr-Nd-Pb isotopes of Monte Amiata volcano, central Italy: evidence for magma mixing between high-K calc-alkaline and leucititic mantle-derivd magmas/doi:/rivista:Italian Journal of Geosciences (Online)/anno:2015/pagina_da:266/pagina_a:290/intervallo_pagine:266–290/volume:134
Monte Amiata is a small volcano composed by trachytic to olivine latitic lava flows and domes emplaced in a very short time between 305 and 231 ka. The main petrographic features are represented by the occurrence of i) abundant rounded magmatic encla
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::33a570cbdba08d08fd40b3f0e87165ec
http://www.cnr.it/prodotto/i/334316
http://www.cnr.it/prodotto/i/334316