Zobrazeno 1 - 10
of 158
pro vyhledávání: '"Riccardo Vannucci"'
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 88, Iss 1 (2023)
Tuffaceous layers of Middle-Triassic age, weakly metamorphosed, are interbedded within a carbonatic succession outcropping near Cogoleto (Voltri Group, Pennidic Zone of the Alps). Volcanic glass, K-feldspar, plagioclase and biotite subordinate, const
Externí odkaz:
https://doaj.org/article/51365a536c284fa0b1d4c4cfc310853d
Autor:
André Ullal, Sergi Aguacil, Riccardo Vannucci, Shen Yang, Joëlle Goyette Pernot, Dusan Licina, Paolo Tombesi
Publikováno v:
Energy and Buildings. 264:112035
Humanitarian tents provide emergency shelter for people displaced by conflict and disaster in diverse climatic conditions. This article compares the thermal performance of two standard humanitarian tents – the Standard Family Tent (SFT) and the Geo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0e657789a575da3b6a9fd1a7ed80652f
https://doi.org/10.1016/j.enbuild.2022.112035
https://doi.org/10.1016/j.enbuild.2022.112035
Publikováno v:
Arabian Journal of Geosciences
Arabian Journal of Geosciences, 2019, 12 (9), ⟨10.1007/s12517-019-4457-2⟩
Arabian Journal Of Geosciences (1866-7511) (Springer Heidelberg), 2019-05, Vol. 12, N. 9, P. 291 (?p.)
Arabian Journal of Geosciences, Springer, 2019, 12 (9), ⟨10.1007/s12517-019-4457-2⟩
Arabian Journal of Geosciences, 2019, 12 (9), ⟨10.1007/s12517-019-4457-2⟩
Arabian Journal Of Geosciences (1866-7511) (Springer Heidelberg), 2019-05, Vol. 12, N. 9, P. 291 (?p.)
Arabian Journal of Geosciences, Springer, 2019, 12 (9), ⟨10.1007/s12517-019-4457-2⟩
Trachyte plugs from the Natash volcanic field have been precisely dated using in situ U-Pb geochronology on zircon grains at similar to 93Ma. Available zircon ages thus suggest that the overall volcanic history at Natash was probably shorter than pre
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3d894ab1bae1685b8e5f85a87b7a08ff
https://hal.uca.fr/hal-02117469/file/75943.pdf
https://hal.uca.fr/hal-02117469/file/75943.pdf
Autor:
Luisa Ottolini, P. M. Nuccio, Federica Schiavi, A. Rosciglione, Eizo Nakamura, Hiroshi Kitagawa, Riccardo Vannucci, Katsura Kobayashi, Antonio Paonita
Publikováno v:
Geochemistry, Geophysics, Geosystems. 16:2109-2126
We present a geochemical study on olivine and clinopyroxene-hosted melt inclusions (MIs) from 2001 to 2006 Etna basaltic lavas and pyroclastites. Three MI suites are distinguished on the basis of trace element fingerprinting. Type-1 MIs (from 2001 Up
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::be2476f0bbb9942897f70291b5dea730
https://doi.org/10.1002/2015gc005786
https://doi.org/10.1002/2015gc005786
Publikováno v:
Lithos
Lithos, 2018, 300-301, pp.136-153. ⟨10.1016/j.lithos.2017.11.037⟩
Lithos, Elsevier, 2018, 300-301, pp.136-153. ⟨10.1016/j.lithos.2017.11.037⟩
Lithos, 2018, 300-301, pp.136-153. ⟨10.1016/j.lithos.2017.11.037⟩
Lithos, Elsevier, 2018, 300-301, pp.136-153. ⟨10.1016/j.lithos.2017.11.037⟩
International audience; A large late Cretaceous (~ 90 Ma) volcanic field (the Natash volcanic province) crops out in southeast Egypt at the northwestern boundary of the Arabian-Nubian shield. The lavas are mainly of alkaline affinity and exhibit a co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bc9a77066393a6e39c1cfc1d36f03bc5
https://hal.uca.fr/hal-01677656/document
https://hal.uca.fr/hal-01677656/document
Autor:
L. Ottolini, E. R. Neumann, Martin J. Whitehouse, M.A: Abu El-Rus, Massimo Tiepolo, Riccardo Vannucci
Publikováno v:
Journal of Petrology. 56:3-31
Mantle xenoliths collected from Fuerteventura, one of the easternmost Canary Islands, exhibit a complex evolutionary history comprising events of depletion, serpentinization, dehydration and melt metasomatism. Each of these events left imprints on bo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::559e0fc96c319cccdf96f791c153f5b1
https://doi.org/10.1093/petrology/egu069
https://doi.org/10.1093/petrology/egu069
Autor:
Vincenzo Brescia Morra, Lorenzo Fedele, Leone Melluso, Michele Lustrino, Riccardo Vannucci, Alberto Zanetti
Publikováno v:
The American mineralogist 100 (2015): 233–249. doi:10.2138/am-2015-4995
info:cnr-pdr/source/autori:Fedele L.; Lustrino M.; Melluso L.; Morra V.; Zanetti A.; Vannucci R./titolo:Trace-element partitioning between plagioclase, alkali feldspar, Ti-magnetite, biotite, apatite, and evolved potassic liquids from Campi Flegrei (Southern Italy)/doi:10.2138%2Fam-2015-4995/rivista:The American mineralogist/anno:2015/pagina_da:233/pagina_a:249/intervallo_pagine:233–249/volume:100
info:cnr-pdr/source/autori:Fedele L.; Lustrino M.; Melluso L.; Morra V.; Zanetti A.; Vannucci R./titolo:Trace-element partitioning between plagioclase, alkali feldspar, Ti-magnetite, biotite, apatite, and evolved potassic liquids from Campi Flegrei (Southern Italy)/doi:10.2138%2Fam-2015-4995/rivista:The American mineralogist/anno:2015/pagina_da:233/pagina_a:249/intervallo_pagine:233–249/volume:100
Partition coefficients (Min/L D ) for a series of geochemically relevant elements have been calculated from combined EMP/LA-ICP-HRMS analyses of plagioclase, alkali feldspar, Ti-magnetite, biotite, apatite, and trachytic/trachyphonolitic melt pairs i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e119302722e27aa1177ff6b9b909bd50
https://doi.org/10.2138/am-2015-4995
https://doi.org/10.2138/am-2015-4995
Autor:
Massimo Tiepolo, Riccardo Vannucci
Publikováno v:
Lithos. :16-20
The continental crust (CC) and the depleted mantle (DM) are generally assumed to be complementary reservoirs within the Earth. However, the mixture between CC and upper mantle does not generate the Nb/Ta and Nb/La ratios of chondrites. A reservoir wi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5087a21118637c591c200bba2edd4cab
https://doi.org/10.1016/j.lithos.2014.07.028
https://doi.org/10.1016/j.lithos.2014.07.028
Autor:
Tomoaki Morishita, Alberto Zanetti, Tommaso Giovanardi, Riccardo Vannucci, Maurizio Mazzucchelli
Publikováno v:
European journal of mineralogy (Internet) 25 (2013): 17–31. doi:10.1127/0935-1221/2013/0025-2251
info:cnr-pdr/source/autori:Giovanardi T. [1], Morishita T. [2], Zanetti A.[3], Mazzucchelli M. [4], Vannucci R. [1]/titolo:Igneous sapphirine as a product of melt-peridotite interactions in the Finero Phlogopite-Peridotite Massif, Western Italian Alps./doi:10.1127%2F0935-1221%2F2013%2F0025-2251/rivista:European journal of mineralogy (Internet)/anno:2013/pagina_da:17/pagina_a:31/intervallo_pagine:17–31/volume:25
info:cnr-pdr/source/autori:Giovanardi T. [1], Morishita T. [2], Zanetti A.[3], Mazzucchelli M. [4], Vannucci R. [1]/titolo:Igneous sapphirine as a product of melt-peridotite interactions in the Finero Phlogopite-Peridotite Massif, Western Italian Alps./doi:10.1127%2F0935-1221%2F2013%2F0025-2251/rivista:European journal of mineralogy (Internet)/anno:2013/pagina_da:17/pagina_a:31/intervallo_pagine:17–31/volume:25
Sapphirine is generally interpreted to be of metamorphic origin in high-MgO-Al2O3 rocks. Igneous sapphirine, i.e. sapphirine crystallised from melt, is very rare. We examined sapphirine-bearing magmatic veins in the Finero Phlogopite-Peridotite Massi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d1707e701eab4f6b50bfb671bb2296be
https://doi.org/10.1127/0935-1221/2013/0025-2251
https://doi.org/10.1127/0935-1221/2013/0025-2251
Publikováno v:
Contributions to Mineralogy and Petrology
Contributions to Mineralogy and Petrology, Springer Verlag, 2012, 163 (6), pp.1011-1031. ⟨10.1007/s00410-011-0713-5⟩
Contributions to mineralogy and petrology 163 (2012): 1011–1031. doi:10.1007/s00410-011-0713-5
info:cnr-pdr/source/autori:Schiavi F. [1]; Kobayashi K. [2]; Nakamura E. [2]; Tiepolo M. [3]; Vannucci R. [1,3]/titolo:Trace element and Pb-B-Li isotope systematics of olivine-hosted melt inclusions: insights into source metasomatism beneath Stromboli (southern Italy)/doi:10.1007%2Fs00410-011-0713-5/rivista:Contributions to mineralogy and petrology/anno:2012/pagina_da:1011/pagina_a:1031/intervallo_pagine:1011–1031/volume:163
Contributions to Mineralogy and Petrology, Springer Verlag, 2012, 163 (6), pp.1011-1031. ⟨10.1007/s00410-011-0713-5⟩
Contributions to mineralogy and petrology 163 (2012): 1011–1031. doi:10.1007/s00410-011-0713-5
info:cnr-pdr/source/autori:Schiavi F. [1]; Kobayashi K. [2]; Nakamura E. [2]; Tiepolo M. [3]; Vannucci R. [1,3]/titolo:Trace element and Pb-B-Li isotope systematics of olivine-hosted melt inclusions: insights into source metasomatism beneath Stromboli (southern Italy)/doi:10.1007%2Fs00410-011-0713-5/rivista:Contributions to mineralogy and petrology/anno:2012/pagina_da:1011/pagina_a:1031/intervallo_pagine:1011–1031/volume:163
We studied the elemental and isotopic (Pb, B and Li isotopes) composition of melt inclusions hosted in highly forsteritic (Fo(83-91)) olivines that were collected from San Bartolo lava and pumice (ST79p, ST82p and ST531p) samples erupted by Stromboli
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9b653a16fab5e2f0d7fb18fb186f79e3
https://doi.org/10.1007/s00410-011-0713-5
https://doi.org/10.1007/s00410-011-0713-5