Výsledky vyhledávání - "Manetti P.(3)"

Extension of a continental lithosphere weakened by impregnation of asthenospheric melts: analogue modelling approach

Autor: Corti G. (1), Bonini M. (1), Innocenti F.(2), Manetti P.(3)

Publikováno v: Ofioliti (Bologna) 30 (2005): 159–159.
info:cnr-pdr/source/autori:Corti G. (1), Bonini M. (1), Innocenti F.(2), Manetti P.(3)/titolo:Extension of a continental lithosphere weakened by impregnation of asthenospheric melts: analogue modelling approach./doi:/rivista:Ofioliti (Bologna)/anno:2005/pagina_da:159/pagina_a:159/intervallo_pagine:159–159/volume:30

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::45edc4d808ba50929df4d5f72e682641
http://www.cnr.it/prodotto/i/111976

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Autor: D'Orazio M. 1), Agostini S. 3), Innocenti F. 1), Haller M.J. 2), Manetti P. 3), Mazzarini F. 3)

Publikováno v: Lithos (Oslo. Print) 57 (2001): 67–89.
info:cnr-pdr/source/autori:D'Orazio M. 1), Agostini S. 3), Innocenti F. 1), Haller M.J. 2), Manetti P. 3), Mazzarini F. 3)/titolo:Slab window-related magmatism from southernmost South America: the Late Miocene mafic volcanics from the Estancia Glencross Area (ca. 52°S, Argentina?Chile)/doi:/rivista:Lithos (Oslo. Print)/anno:2001/pagina_da:67/pagina_a:89/intervallo_pagine:67–89/volume:57

The Estancia Glencross Area EGA volcanic rocks form a series of five isolated buttes located at the southern end ca. 52°S of the discontinuous belt of Cenozoic basaltic lava formations occurring in the extra-Andean Patagonia. EGA volcanics are subal

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::9ccce3f9ee49d8de304ccf621d6a86a6
http://www.cnr.it/prodotto/i/29050

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Provenance of Tertiary volcanoclastic sediment in NW Thrace (Bulgaria): Evidence from detrital amphibole and pyroxene geochemistry

Autor: David Riley, Piero Manetti, Raya Raycheva, Salvatore Critelli, Andrea Orlando, Peter Marchev, Luca Caracciolo

Publikováno v: Sedimentary Geology 336 (2016): 120–137. doi:10.1016/j.sedgeo.2016.01.026
info:cnr-pdr/source/autori:Caracciolo L.[1], Orlando A.[2], Marchev P.[3], Critelli S.[4], Manetti P.[3], Raycheva R.[3], Riley D.[1]/titolo:Provenance of Tertiary volcanoclastic sediment in NW Thrace (Bulgaria): Evidence from detrital amphibole and pyroxene geochemistry/doi:10.1016%2Fj.sedgeo.2016.01.026/rivista:Sedimentary Geology/anno:2016/pagina_da:120/pagina_a:137/intervallo_pagine:120–137/volume:336

Detrital heavy mineral and bulk rock geochemistry and a review of sandstone petrographic data have been used to investigate the post-collisional effusive magmatism that followed the closure of the Vardar Ocean and the generation of volcanic sediments

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::62293d91555d00d805ab6de9feea6ef9
https://doi.org/10.1016/j.sedgeo.2016.01.026

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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

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

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

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Tertiary high-Mg volcanic rocks from western Anatolia and their geodynamic significance for the evolution of the Aegean area

Autor: Agostini, S, Doglioni, Carlo, Innocenti, F, Manetti, P, Savascin, M. Y. TONARINI S.

Publikováno v: The South Aegean Active Volcanic Arc Present Knowledge and Future Perspectives, edited by M. Fytikas; G. Vougioukalakis, pp. 345–362, 2005
info:cnr-pdr/source/autori:Agostini S.(1,3); Doglioni C.(2); Innocenti F.(1); Manetti P.(3); Savascin M.Y.(4), Tonarini S.(3)/titolo:Tertiary high-Mg volcanic rocks from western Anatolia and their geodynamic significance for the evolution of the Aegean area./titolo_volume:The South Aegean Active Volcanic Arc Present Knowledge and Future Perspectives/curatori_volume:M. Fytikas; G. Vougioukalakis/editore:/anno:2005

Scattered Late Miocene high-Mg basaltic andesites to dacites can be found in Western Anatolia. These rocks display Mg#>65, high Ca0/A12O3 ratio, low alkalies and TiO2 contents. Trace element distribution shows typical orogenic signature with higher v

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::5a9cfb702851d40c378ec30590dd9d82
http://www.cnr.it/prodotto/i/135738

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