Zobrazeno 1 - 8
of 8
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
Autor:
Horst Zwingmann, Neil S. Mancktelow, Giovanni Luca Cardello, Gianfranco Di Vincenzo, Giovanna Giorgetti
Publikováno v:
Journal of structural geology 126 (2019): 338–356. doi:10.1016/j.jsg.2019.06.014
info:cnr-pdr/source/autori:Cardello G.[1,2], Di Vincenzo G.[3], Giorgetti G.[4], Zwingmann H.[5], Mancktelow N.[2]/titolo:Initiation and development of the Pennine Basal Thrust (Swiss Alps): a structural and geochronological study of an exhumed megathrust/doi:10.1016%2Fj.jsg.2019.06.014/rivista:Journal of structural geology/anno:2019/pagina_da:338/pagina_a:356/intervallo_pagine:338–356/volume:126
info:cnr-pdr/source/autori:Cardello G.[1,2], Di Vincenzo G.[3], Giorgetti G.[4], Zwingmann H.[5], Mancktelow N.[2]/titolo:Initiation and development of the Pennine Basal Thrust (Swiss Alps): a structural and geochronological study of an exhumed megathrust/doi:10.1016%2Fj.jsg.2019.06.014/rivista:Journal of structural geology/anno:2019/pagina_da:338/pagina_a:356/intervallo_pagine:338–356/volume:126
The Pennine Basal Thrust (PBT) is an exhumed megathrust developed during continental collision from late Eocene to Miocene. To trace its evolution, five samples, with indications for up to three microstructurally diachronous white-mica generations, w
Autor:
R.E. Nyland, K.S. Panter, S. Rocchi, G. Di Vincenzo, P. Del Carlo, M. Tiepolo, B. Field, P. Gorsevski
Publikováno v:
Journal of volcanology and geothermal research 250 (2013): 106–128.
info:cnr-pdr/source/autori:Nyland R. [1]; Panter K. [1]; Rocchi S. [2]; Di Vincenzo G. [3]; Del Carlo P. [4]; Tiepolo M. [5]; Field B. [6]; Gorsevski P. [1]/titolo:Volcanic activity and its link to glaciation cycles: Single-grain age and geochemistry of early to middle miocene volcanic glass from ANDRILL AND-2A core, Antarctica./doi:/rivista:Journal of volcanology and geothermal research/anno:2013/pagina_da:106/pagina_a:128/intervallo_pagine:106–128/volume:250
info:cnr-pdr/source/autori:Nyland R. [1]; Panter K. [1]; Rocchi S. [2]; Di Vincenzo G. [3]; Del Carlo P. [4]; Tiepolo M. [5]; Field B. [6]; Gorsevski P. [1]/titolo:Volcanic activity and its link to glaciation cycles: Single-grain age and geochemistry of early to middle miocene volcanic glass from ANDRILL AND-2A core, Antarctica./doi:/rivista:Journal of volcanology and geothermal research/anno:2013/pagina_da:106/pagina_a:128/intervallo_pagine:106–128/volume:250
In the frame of the ANtarctic DRILLing Program, volcanic glass fragments were collected from the AND-2A core between ~ 354 and 765 m below sea floor (mbsf) as accumulations (5–70 vol.%) within sediments. Here, we present the physical characteristic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7438f47b13a34cce5df9accca88c4b83
https://publications.cnr.it/doc/209925
https://publications.cnr.it/doc/209925
Publikováno v:
Sedimentary Geology 243-244 (2012): 117–129.
info:cnr-pdr/source/autori:D'Atri A. [1]; Zuffa G. G. [1]; Cavazza W. [1]; Okay A. [2]; Di Vincenzo G. [3]/titolo:Detrital supply from subduction%2Faccretion complexes to the Eocene-Oligocene post-collisional southern Thrace Basin (NW Turkey and NE Greece)./doi:/rivista:Sedimentary Geology/anno:2012/pagina_da:117/pagina_a:129/intervallo_pagine:117–129/volume:243-244
info:cnr-pdr/source/autori:D'Atri A. [1]; Zuffa G. G. [1]; Cavazza W. [1]; Okay A. [2]; Di Vincenzo G. [3]/titolo:Detrital supply from subduction%2Faccretion complexes to the Eocene-Oligocene post-collisional southern Thrace Basin (NW Turkey and NE Greece)./doi:/rivista:Sedimentary Geology/anno:2012/pagina_da:117/pagina_a:129/intervallo_pagine:117–129/volume:243-244
The Thrace Basin is a large, mostly Eocene–Oligocene post-collisional sedimentary basin which developed following the closure of the Vardar–Izmir–Ankara oceanic domain (latest Cretaceous–Paleocene). Sandstone petrologic data (framework and he
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e86d45d1e5d58c95fedaec452b002366
http://scienceserver.cilea.it/cgi-bin/sciserv.pl?collection=journals&journal=00370738
http://scienceserver.cilea.it/cgi-bin/sciserv.pl?collection=journals&journal=00370738
Publikováno v:
Scopus-Elsevier
Periodico di mineralogia (Testo stamp.) 73 (2004): 73–83.
info:cnr-pdr/source/autori:Ricci C.A. (1), Carosi R. (2), Di Vincenzo G. (3), Franceschelli M.(4), Palmeri R. (5)/titolo:Unravelling the tectono-metamorphic evolution of medium-pressure rocks from collision to exhumation of the Variscan basement of NE Sardinia (Italy): a review/doi:/rivista:Periodico di mineralogia (Testo stamp.)/anno:2004/pagina_da:73/pagina_a:83/intervallo_pagine:73–83/volume:73
Periodico di mineralogia (Testo stamp.) 73 (2004): 73–83.
info:cnr-pdr/source/autori:Ricci C.A. (1), Carosi R. (2), Di Vincenzo G. (3), Franceschelli M.(4), Palmeri R. (5)/titolo:Unravelling the tectono-metamorphic evolution of medium-pressure rocks from collision to exhumation of the Variscan basement of NE Sardinia (Italy): a review/doi:/rivista:Periodico di mineralogia (Testo stamp.)/anno:2004/pagina_da:73/pagina_a:83/intervallo_pagine:73–83/volume:73
The basement of NE Sardinia consists of magmatic-sedimentary sequences affected by a polyphase deformation (D1, D2, D3 and D4)) and an increase in the metamorphic grade northwards, toward the inner zone of belt. D1 is mainly detected in the low-grade
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::095f5dc1fbe4c81485301497b17fcc72
http://www.scopus.com/inward/record.url?eid=2-s2.0-33745146782&partnerID=MN8TOARS
http://www.scopus.com/inward/record.url?eid=2-s2.0-33745146782&partnerID=MN8TOARS
Autor:
Ira A. Glazier, William P. Filby
Italians to America is the first indexed reference work devoted to Italian immigrants to the United States. This series contains passenger list information in chronological order on the first major wave of Italian migration during the last two decade