Výsledky vyhledávání - "Pinarelli L.[1]"

Mantle source heterogeneity in subduction zones: constraints from elemental and isotope (Sr, Nd, and Pb) data on Vulcano Island, Aeolian Archipelago, Italy

Autor: Pinarelli L.[1], Gioncada A.[2], Capaccioni B.[3], Vaselli O.[1, Downes H.[5]

Publikováno v: Mineralogy and petrology (Internet) 113 (2019): 39–60. doi:10.1007/s00710-018-0640-5
info:cnr-pdr/source/autori:Pinarelli L.[1], Gioncada A.[2], Capaccioni B.[3], Vaselli O.[1,4], Downes H.[5]/titolo:Mantle source heterogeinity in subduction zones: constrains from elemental and isotope (Sr, Nd and Pb) data on Vulcano Island, Aeolian Archipelago, Italy/doi:10.1007%2Fs00710-018-0640-5/rivista:Mineralogy and petrology (Internet)/anno:2019/pagina_da:39/pagina_a:60/intervallo_pagine:39–60/volume:113

Vulcano is part of the Aeolian volcanic arc in the southern Tyrrhenian Sea. Its products were emplaced through multiple episodes of edifice building and collapse since about 120 ka B.P. to present. A major discontinuity in the activity occurred after

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e684169164391e9bb90aa223446bfdef
https://doi.org/10.1007/s00710-018-0640-5

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Mineral resources in the Red Sea/Gulf of Aden: Polymetallic-Barite mineralizations at Wadi Masilah Basin (Yemen)

Autor: Pinarelli L.[1], Mattash M.A.[2]

Publikováno v: Red Sea: Historical Significance, Properties and Economic Importance, edited by Robbins D. (editor), pp. 46–76. Hauppauge: Nova Publishers, 2018
info:cnr-pdr/source/autori:Pinarelli L.[1], Mattash M.A.[2]/titolo:Mineral resources in the Red Sea%2FGulf of Aden: Polymetallic-Barite mineralizations at Wadi Masilah Basin (Yemen)./titolo_volume:Red Sea: Historical Significance, Properties and Economic Importance/curatori_volume:Robbins D. (editor)/editore: /anno:2018

Yemen is characterized by a considerable number of metallic and non-metallic raw materials, including base metals, precious metals, and dimension stones. The Wadi Masilah Basin, in the southeasternmost part of Yemen, hosts very promising base metal a

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::3c2006dcb97c88148e2c4050dfb74a3d
https://publications.cnr.it/doc/386424

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Il magnetismo della Toscana: 'un rebus avvolto in un mistero dentro un enigma'

Autor: Pinarelli L.[1], Peccerillo A. [2]

Publikováno v: Codice Armonico 2018-Settimo Congresso di Scienze Naturali. Ambiente Toscano., edited by Lenzi A., Leoni L., Brizzi B., Piombanti P., Baldacci C., Santinelli M., Domenici V., Del Santi C., Lucchesi P., Centrella E. (eds.), pp. 56–63. Pisa: ETS, 2018
info:cnr-pdr/source/autori:Pinarelli L.[1], Peccerillo A. [2]/titolo:Il magnetismo della Toscana: "un rebus avvolto in un mistero dentro un enigma"./titolo_volume:Codice Armonico 2018-Settimo Congresso di Scienze Naturali. Ambiente Toscano./curatori_volume:Lenzi A., Leoni L., Brizzi B., Piombanti P., Baldacci C., Santinelli M., Domenici V., Del Santi C., Lucchesi P., Centrella E. (eds.)/editore: /anno:2018

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Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::07f6ccaf35927423ff43c7991a3dd6c3
http://www.cnr.it/prodotto/i/392812

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Major, trace element, and Sr isotope geochemistry of surface and ground waters in the Chiavenna Valley (Sondrio, Northern Italy)

Autor: Pinarelli L.[1], Nisi B.[1, Vaselli O.[1, Minissale A.[1], Buccianti A.[1, Tassi F.[1

Publikováno v: Rendiconti online Società Geologica Italiana 30 (2014): 62–65. doi:10.3301/ROL.2014.13
info:cnr-pdr/source/autori:Pinarelli L.[1], Nisi B.[1,2], Vaselli O.[1,3], Minissale A.[1], Buccianti A.[1,3], Tassi F.[1,3]/titolo:Major, trace element, and Sr isotope geochemistry of surface and ground waters in the Chiavenna Valley (Sondrio, Northern Italy)/doi:10.3301%2FROL.2014.13/rivista:Rendiconti online Società Geologica Italiana/anno:2014/pagina_da:62/pagina_a:65/intervallo_pagine:62–65/volume:30

The Chiavenna Valley (Sondrio, Northern Italy) is located in the Central Alps and is elongated along a NNW-SSE direction. Geologically, it consists of a poly-metamorphic sequence, which includes metasediments, metagranitoids, and ophiolites, intruded

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4947c905152297bba61e909d8f6882e1
https://doi.org/10.3301/rol.2014.13

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Crust and Mantle Contributions to Orogenic Granitoid Magmatism: The Case of Tertiary Magmatism of Alps (Italy)

Autor: Pinarelli L. [1], Peccerillo A., Donati C.

Publikováno v: Granite: Occurrence, Mineralogy and Origin, edited by Blasik M. and Hanika B. (Eds.), pp. 57–78. Hauppauge: Nova Science Publishers, 2012
info:cnr-pdr/source/autori:Pinarelli L. [1]; Peccerillo A.; Donati C./titolo:Crust and Mantle Contributions to Orogenic Granitoid Magmatism: The Case of Tertiary Magmatism of Alps (Italy)/titolo_volume:Granite: Occurrence, Mineralogy and Origin/curatori_volume:Blasik M. and Hanika B. (Eds.)/editore: /anno:2012

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::0f8ad8fe526b5a683034716d103c115e
https://publications.cnr.it/doc/208679

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