Zobrazeno 1 - 3
of 3
pro vyhledávání: '"Rocchi S. (1)"'
Publikováno v:
International journal of earth sciences (1999, Internet) 107 (2018): 1343–1355.
info:cnr-pdr/source/autori:Vezzoni S.[1], Rocchi S.[1], Dini A.[2]/titolo:Lateral extrusion of a thermally weakened pluton overburden (Campiglia Maritima, Tuscany)/doi:/rivista:International journal of earth sciences (1999, Internet)/anno:2018/pagina_da:1343/pagina_a:1355/intervallo_pagine:1343–1355/volume:107
info:cnr-pdr/source/autori:Vezzoni S.[1], Rocchi S.[1], Dini A.[2]/titolo:Lateral extrusion of a thermally weakened pluton overburden (Campiglia Maritima, Tuscany)/doi:/rivista:International journal of earth sciences (1999, Internet)/anno:2018/pagina_da:1343/pagina_a:1355/intervallo_pagine:1343–1355/volume:107
The ascent and emplacement of magmas in the upper crust modify the local pre-existing thermal and rheological settings. Such changes have important effects in producing anomalous structures, mass extrusion, rock fracturing, and in some conditions, hy
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::89628b8803033fc109bc62e0f421e250
https://publications.cnr.it/doc/392741
https://publications.cnr.it/doc/392741
Publikováno v:
Ofioliti (Bologna) 38 (2013): 15–28. doi:10.4454/ofioliti.v38i1.413
info:cnr-pdr/source/autori:Donatio D.[1], Marroni M.[1,2], Rocchi S.[1]/titolo:Serpentinization history in mantle section from a fossil slow-spreading ridge sequence: Evidences from Pomaia quarry (Southern Tuscany, Italy)/doi:10.4454%2Fofioliti.v38i1.413/rivista:Ofioliti (Bologna)/anno:2013/pagina_da:15/pagina_a:28/intervallo_pagine:15–28/volume:38
info:cnr-pdr/source/autori:Donatio D.[1], Marroni M.[1,2], Rocchi S.[1]/titolo:Serpentinization history in mantle section from a fossil slow-spreading ridge sequence: Evidences from Pomaia quarry (Southern Tuscany, Italy)/doi:10.4454%2Fofioliti.v38i1.413/rivista:Ofioliti (Bologna)/anno:2013/pagina_da:15/pagina_a:28/intervallo_pagine:15–28/volume:38
n the Pomaia quarry (Southern Tuscany, Italy) a mantle section consisting of peridotites belonging to the Internal Ligurian units is exposed. This mantle section, that is regarded as representative of the Jurassic oceanic lithosphere of the Ligure-Pi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::4a74ca62290f67d59df5bc534a3b6e99
http://www.cnr.it/prodotto/i/456614
http://www.cnr.it/prodotto/i/456614
Publikováno v:
edited by Storti F., Holdsworth R.E., Salvini F., pp. 145–158. London: Geological society, 2003
info:cnr-pdr/source/autori:Rocchi S. (1), Storti F. (2), Di Vincenzo G. (3), Rossetti F. (2)/titolo:Intraplate strike-slip tectonics as alternative to mantle plume activity for the Cenozoic rift magmatism in the Ross Sea region Antarctica./titolo_volume:/curatori_volume:Storti F., Holdsworth R.E., Salvini F./editore: /anno:2003
info:cnr-pdr/source/autori:Rocchi S. (1), Storti F. (2), Di Vincenzo G. (3), Rossetti F. (2)/titolo:Intraplate strike-slip tectonics as alternative to mantle plume activity for the Cenozoic rift magmatism in the Ross Sea region Antarctica./titolo_volume:/curatori_volume:Storti F., Holdsworth R.E., Salvini F./editore: /anno:2003
The West Antarctic Rift System is one of the largest areas of crustal extension in the world. Current interpretations on its driving mechanisms mostly rely on the occurrence of one or more mantle plumes, active during the Cenozoic or the Mesozoic. Re
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::b97a4eca7213728196bf7b31ecc5663a
https://publications.cnr.it/doc/135722
https://publications.cnr.it/doc/135722