Zobrazeno 1 - 3
of 3
pro vyhledávání: '"Di Vincenzo G.[3]"'
Publikováno v:
Lithos (Oslo. Print) 300-301 (2018): 361–377.
info:cnr-pdr/source/autori:Palmeri R.[1], Godard G.[2], Di Vincenzo G.[3], Sandroni S. [1], Talarico F. [1,4]/titolo:High-pressure granulite-facies metamorphism in central Dronning Maud Land (East Antarctica): Implications for Gondwana assembly/doi:/rivista:Lithos (Oslo. Print)/anno:2018/pagina_da:361/pagina_a:377/intervallo_pagine:361–377/volume:300-301
info:cnr-pdr/source/autori:Palmeri R.[1], Godard G.[2], Di Vincenzo G.[3], Sandroni S. [1], Talarico F. [1,4]/titolo:High-pressure granulite-facies metamorphism in central Dronning Maud Land (East Antarctica): Implications for Gondwana assembly/doi:/rivista:Lithos (Oslo. Print)/anno:2018/pagina_da:361/pagina_a:377/intervallo_pagine:361–377/volume:300-301
Central Dronning Maud Land (DML; East Antarctica) is located in a key region of the Gondwana supercontinent. The Conradgebirge area (central DML) consists of orthogneisses, derived from both volcanic and plutonic protoliths, and minor metasedimentary
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::7784ccc46cfa7a770e86c1176963caba
https://publications.cnr.it/doc/386547
https://publications.cnr.it/doc/386547
Publikováno v:
Palaeogeography, palaeoclimatology, palaeoecology 307 (2011): 129–149.
info:cnr-pdr/source/autori:Smellie, J.L. (1); Rocchi, S. (2); Gemelli, M. (2); Di Vincenzo, G. (3); Armienti, P. (2)/titolo:A thin predominantly cold-based Late Miocene East Antarctic ice sheet inferred from glaciovolcanic sequences in northern Victoria land/doi:/rivista:Palaeogeography, palaeoclimatology, palaeoecology/anno:2011/pagina_da:129/pagina_a:149/intervallo_pagine:129–149/volume:307
info:cnr-pdr/source/autori:Smellie, J.L. (1); Rocchi, S. (2); Gemelli, M. (2); Di Vincenzo, G. (3); Armienti, P. (2)/titolo:A thin predominantly cold-based Late Miocene East Antarctic ice sheet inferred from glaciovolcanic sequences in northern Victoria land/doi:/rivista:Palaeogeography, palaeoclimatology, palaeoecology/anno:2011/pagina_da:129/pagina_a:149/intervallo_pagine:129–149/volume:307
Glaciovolcanic sequences are widespread in northern Victoria Land and their interpretation enables estimates of past ice thicknesses and other defining parameters of the coeval ice sheet to be made with considerable certainty. The terrestrial sequenc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::6b772a7b244115eeafeec460bb9ec9c5
http://scienceserver.cilea.it/cgi-bin/sciserv.pl?collection=journals&journal=00310182
http://scienceserver.cilea.it/cgi-bin/sciserv.pl?collection=journals&journal=00310182
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