Zobrazeno 1 - 2
of 2
pro vyhledávání: '"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
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
http://www.cnr.it/prodotto/i/111976
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
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
http://www.cnr.it/prodotto/i/29050