Zobrazeno 1 - 2
of 2
pro vyhledávání: '"Boari E.[1]"'
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
Autor:
Massimo Mattei, Francesca Cifelli, Sandro Conticelli, Simone Tommasini, Guido Giordano, Marinella A. Laurenzi, Leone Melluso, Giulia Perini, Elena Boari, Riccardo Avanzinelli
Publikováno v:
Journal of the virtual explorer (Online) 36 (2010). doi:10.3809/jvirtex.2010.00251
info:cnr-pdr/source/autori:Conticelli S. (1)(2); Laurenzi M.A. (3); Giordano G. (4); Mattei M. (4); Avanzinelli R. (1); Melluso L. (5); Tommasini S. (1); Boari E. (1); Cifelli F. (4); Perini G. (6)/titolo:Leucite-bearing (kamafugitic%2Fleucititic) and-free (lamproitic) ultrapotassic rocks and associated shoshonites from Italy: constraints on petrogenesis and geodynamics/doi:10.3809%2Fjvirtex.2010.00251/rivista:Journal of the virtual explorer (Online)/anno:2010/pagina_da:/pagina_a:/intervallo_pagine:/volume:36
info:cnr-pdr/source/autori:Conticelli S. (1)(2); Laurenzi M.A. (3); Giordano G. (4); Mattei M. (4); Avanzinelli R. (1); Melluso L. (5); Tommasini S. (1); Boari E. (1); Cifelli F. (4); Perini G. (6)/titolo:Leucite-bearing (kamafugitic%2Fleucititic) and-free (lamproitic) ultrapotassic rocks and associated shoshonites from Italy: constraints on petrogenesis and geodynamics/doi:10.3809%2Fjvirtex.2010.00251/rivista:Journal of the virtual explorer (Online)/anno:2010/pagina_da:/pagina_a:/intervallo_pagine:/volume:36
In Italy and surroundings, leucite-free (i.e., lamproites), leucite-bearing (i.e., kamafugites, leucitites, plagioclase-leucitites), and haüyne-bearing (i.e., haüynites, haüyne-leucitites) ultrapotassic igneous rocks have been recorded from Oli
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::76a47be5b4beb97b6dd4864b793bfa56
https://doi.org/10.3809/jvirtex.2010.00251
https://doi.org/10.3809/jvirtex.2010.00251
