Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Natali C.[1]"'
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:
Marchina C.[1], Bianchini G.[1, Natali C.[1], Pennisi M.[2], Colombani N.[3], Tassinari R.[1], Knoeller K.[4]
Publikováno v:
Environmental science and pollution research international 22 (2015): 5184–5203. doi:10.1007/s11356-014-3750-6
info:cnr-pdr/source/autori:Marchina C.[1], Bianchini G.[1,2], Natali C.[1], Pennisi M.[2], Colombani N.[3], Tassinari R.[1], Knoeller K.[4]/titolo:The Po river water from the Alps to the Adriatic Sea (Italy): new insights from geochemical and isotopic (delta18O-deltaD) data/doi:10.1007%2Fs11356-014-3750-6/rivista:Environmental science and pollution research international/anno:2015/pagina_da:5184/pagina_a:5203/intervallo_pagine:5184–5203/volume:22
info:cnr-pdr/source/autori:Marchina C.[1], Bianchini G.[1,2], Natali C.[1], Pennisi M.[2], Colombani N.[3], Tassinari R.[1], Knoeller K.[4]/titolo:The Po river water from the Alps to the Adriatic Sea (Italy): new insights from geochemical and isotopic (delta18O-deltaD) data/doi:10.1007%2Fs11356-014-3750-6/rivista:Environmental science and pollution research international/anno:2015/pagina_da:5184/pagina_a:5203/intervallo_pagine:5184–5203/volume:22
Although the Po river is the most important fluvial system of Northern Italy, the systematic geochemical and isotopic investigations of its water are rare and were never reported for the whole basin. The present contribution aims to fill this knowled
Publikováno v:
Chemical Geology
Chemical Geology, Elsevier, 2014, 386, pp.49-58. ⟨10.1016/j.chemgeo.2014.07.024⟩
Chemical Geology, 2014, 386, pp.49-58. ⟨10.1016/j.chemgeo.2014.07.024⟩
Chemical geology 386 (2014): 49–58. doi:10.1016/j.chemgeo.2014.07.024
info:cnr-pdr/source/autori:Bianchini G.[1,2], Bryce J.G.[3], Blichert-Toft J.[4], Beccaluva L.[1], Natali C.[1]/titolo:Mantle dynamics and secular variations beneath the East African Rift: Insights from peridotite xenoliths (Mega, Ethiopia)/doi:10.1016%2Fj.chemgeo.2014.07.024/rivista:Chemical geology/anno:2014/pagina_da:49/pagina_a:58/intervallo_pagine:49–58/volume:386
Chemical Geology, Elsevier, 2014, 386, pp.49-58. ⟨10.1016/j.chemgeo.2014.07.024⟩
Chemical Geology, 2014, 386, pp.49-58. ⟨10.1016/j.chemgeo.2014.07.024⟩
Chemical geology 386 (2014): 49–58. doi:10.1016/j.chemgeo.2014.07.024
info:cnr-pdr/source/autori:Bianchini G.[1,2], Bryce J.G.[3], Blichert-Toft J.[4], Beccaluva L.[1], Natali C.[1]/titolo:Mantle dynamics and secular variations beneath the East African Rift: Insights from peridotite xenoliths (Mega, Ethiopia)/doi:10.1016%2Fj.chemgeo.2014.07.024/rivista:Chemical geology/anno:2014/pagina_da:49/pagina_a:58/intervallo_pagine:49–58/volume:386
Segments of the Main Ethiopian Rift (MER), a key sector of the East African Rift (EAR) linking the Afar and Turkana depressions, record different stages of lithospheric evolution from initiation to continental break- up and incipient oceanic spreadin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1fcacaebb91a638365f131b2240350bd
https://hal.archives-ouvertes.fr/hal-02110410
https://hal.archives-ouvertes.fr/hal-02110410
Publikováno v:
Ofioliti (Bologna) 38 (2013): 1–14. doi:10.4454/ofioliti.v38i1.412
info:cnr-pdr/source/autori:Bianchini G.[1], Di Giuseppe D.[1], Natali C.[1,2], Beccaluva L.[1]/titolo:Ophiolite inheritance in the Po Plain sediments: Insights on heavy metals distribution and risk assessment/doi:10.4454%2Fofioliti.v38i1.412/rivista:Ofioliti (Bologna)/anno:2013/pagina_da:1/pagina_a:14/intervallo_pagine:1–14/volume:38
info:cnr-pdr/source/autori:Bianchini G.[1], Di Giuseppe D.[1], Natali C.[1,2], Beccaluva L.[1]/titolo:Ophiolite inheritance in the Po Plain sediments: Insights on heavy metals distribution and risk assessment/doi:10.4454%2Fofioliti.v38i1.412/rivista:Ofioliti (Bologna)/anno:2013/pagina_da:1/pagina_a:14/intervallo_pagine:1–14/volume:38
High heavy metals backgrounds, in particular chromium and nickel, are renowned in soils and sediments of the Po Plain. New XRF data, synthetized in geo-referenced geochemical maps, emphasize that the anomalously high Cr-Ni backgrounds are related to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::a2b4d8a3b0287ecaf3dfb1219bc1873e
https://publications.cnr.it/doc/456597
https://publications.cnr.it/doc/456597
Publikováno v:
Lithos (Oslo. Print) 180-181 (2013): 128–137. doi:10.1016/j.lithos.2013.08.006
info:cnr-pdr/source/autori:Beccaluva L.[1], Bianchini G.[1,2], Mameli P.[3], Natali C.[1,2]/titolo:Miocene shoshonite volcanism in Sardinia: Implications for magma sources and geodynamic evolution of the central-western Mediterranean/doi:10.1016%2Fj.lithos.2013.08.006/rivista:Lithos (Oslo. Print)/anno:2013/pagina_da:128/pagina_a:137/intervallo_pagine:128–137/volume:180-181
info:cnr-pdr/source/autori:Beccaluva L.[1], Bianchini G.[1,2], Mameli P.[3], Natali C.[1,2]/titolo:Miocene shoshonite volcanism in Sardinia: Implications for magma sources and geodynamic evolution of the central-western Mediterranean/doi:10.1016%2Fj.lithos.2013.08.006/rivista:Lithos (Oslo. Print)/anno:2013/pagina_da:128/pagina_a:137/intervallo_pagine:128–137/volume:180-181
In this paper we document the existence of a Miocene shoshonite (SHO) volcanism in Northern Sardinia (Anglona). This occurrence completes the spectrum of orogenic magmas related to the subduction process which developed from the Eocene along the Pala
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9cef8f4f7f0de50d44d700c378746b72
http://hdl.handle.net/11392/1896610
http://hdl.handle.net/11392/1896610
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. 257–266, 2013
info:cnr-pdr/source/autori:Gadikota G.[2], Natali C. [1], Boschi C. [1], Park A.-H. A. [2]/titolo:Carbonation of abestos for permanent storage of anthropogenic CO2./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
info:cnr-pdr/source/autori:Gadikota G.[2], Natali C. [1], Boschi C. [1], Park A.-H. A. [2]/titolo:Carbonation of abestos for permanent storage of anthropogenic CO2./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
Asbestos Containing Material (ACM) has long been recognized as hazardous waste due to the presence of chrysotile. Chrysotile ((Mg, Fe)3Si2O5(OH)4)), a natural phyllosilicate that belongs to the serpentine group has a fibrous crystal structure that pr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::6d6b67eeea8f64156df09810c59517c5
https://publications.cnr.it/doc/265348
https://publications.cnr.it/doc/265348
Publikováno v:
Contributions to mineralogy and petrology (Internet) 166 (2013): 351–370. doi:10.1007/s00410-013-0879-0
info:cnr-pdr/source/autori:Natali C. [1], Beccaluva L. [1], Bianchini G. [1, 2], Siena F. [1]/titolo:The Axum-Adwa basalt-trachyte complex: a late magmatic activity at the periphery of the Afar plume./doi:10.1007%2Fs00410-013-0879-0/rivista:Contributions to mineralogy and petrology (Internet)/anno:2013/pagina_da:351/pagina_a:370/intervallo_pagine:351–370/volume:166
info:cnr-pdr/source/autori:Natali C. [1], Beccaluva L. [1], Bianchini G. [1, 2], Siena F. [1]/titolo:The Axum-Adwa basalt-trachyte complex: a late magmatic activity at the periphery of the Afar plume./doi:10.1007%2Fs00410-013-0879-0/rivista:Contributions to mineralogy and petrology (Internet)/anno:2013/pagina_da:351/pagina_a:370/intervallo_pagine:351–370/volume:166
The Axum–Adwa igneous complex consists of a basalt–trachyte (syenite) suite emplaced at the northern periphery of the Ethiopian plateau, after the paroxysmal eruption of the Oligocene (ca 30 Ma) continental flood basalts (CFB), which is related t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8299e38883f175cb5010b7d823c476fd