Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Ribolini A. [1]"'
Autor:
Bini M.[1, Isola I.[2, 3] Zanchetta G.[1, 2] Pappalardo M.[1], Ribolini A.[1], Ragaini L.[1], Baroni C.[1, Boretto G.[4], Fuck E.[5], Morigi C.[1], Salvatore M.C.[1, Bassi D.[6] Marzaioli F.[7], Terrasi F. [7]
Publikováno v:
SEDICI (UNLP)
Universidad Nacional de La Plata
instacron:UNLP
Holocene (Lond. Online) 28 (2018): 56–64. doi:10.1177/0959683617714596
info:cnr-pdr/source/autori:Bini M.[1,2], Isola I.[2,3] Zanchetta G.[1,2] Pappalardo M.[1], Ribolini A.[1], Ragaini L.[1], Baroni C.[1,3], Boretto G.[4], Fuck E.[5], Morigi C.[1], Salvatore M.C.[1,3], Bassi D.[6] Marzaioli F.[7], Terrasi F. [7]/titolo:Mid-Holocene relative sea-level changes along Atlantic Patagonia: New data from Camarones, Chubut, Argentina/doi:10.1177%2F0959683617714596/rivista:Holocene (Lond. Online)/anno:2018/pagina_da:56/pagina_a:64/intervallo_pagine:56–64/volume:28
Universidad Nacional de La Plata
instacron:UNLP
Holocene (Lond. Online) 28 (2018): 56–64. doi:10.1177/0959683617714596
info:cnr-pdr/source/autori:Bini M.[1,2], Isola I.[2,3] Zanchetta G.[1,2] Pappalardo M.[1], Ribolini A.[1], Ragaini L.[1], Baroni C.[1,3], Boretto G.[4], Fuck E.[5], Morigi C.[1], Salvatore M.C.[1,3], Bassi D.[6] Marzaioli F.[7], Terrasi F. [7]/titolo:Mid-Holocene relative sea-level changes along Atlantic Patagonia: New data from Camarones, Chubut, Argentina/doi:10.1177%2F0959683617714596/rivista:Holocene (Lond. Online)/anno:2018/pagina_da:56/pagina_a:64/intervallo_pagine:56–64/volume:28
This paper concerns the relative sea-level changes associated with the Atlantic Patagonian coast derived from sea-level index points whose elevation was determined by a differential global position system (DGPS). Bio encrustations from outcrops locat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2082dd8589942efb90b8094c84bdc18a
http://hdl.handle.net/11392/2381984
http://hdl.handle.net/11392/2381984
Autor:
Zanchetta G.[1, 2, Bini M.[1], Isola I.[2], Regattieri E.[4, Ribolini A.[1], Milevski I.[6], Sulpizio R.[7
Publikováno v:
Italian Journal of Geosciences (Testo stamp.) 136 (2017): 198–205. doi:10.3301/IJG.2016.16
info:cnr-pdr/source/autori:Zanchetta G.[1,2,3], Bini M.[1], Isola I.[2], Regattieri E.[4,5], Ribolini A.[1], Milevski I.[6], Sulpizio R.[7,8]/titolo:New findings of the Campanian Ignimbrite ash within slope deposits of the Treska valley (former Yugoslav Republic of Macedonia)/doi:10.3301%2FIJG.2016.16/rivista:Italian Journal of Geosciences (Testo stamp.)/anno:2017/pagina_da:198/pagina_a:205/intervallo_pagine:198–205/volume:136
info:cnr-pdr/source/autori:Zanchetta G.[1,2,3], Bini M.[1], Isola I.[2], Regattieri E.[4,5], Ribolini A.[1], Milevski I.[6], Sulpizio R.[7,8]/titolo:New findings of the Campanian Ignimbrite ash within slope deposits of the Treska valley (former Yugoslav Republic of Macedonia)/doi:10.3301%2FIJG.2016.16/rivista:Italian Journal of Geosciences (Testo stamp.)/anno:2017/pagina_da:198/pagina_a:205/intervallo_pagine:198–205/volume:136
In this paper, we describe the first finding of the campanian Ignimbrite tephra layer in a subaerial succession in the Former Yugoslav republic of Macedonia. the tephra is interbedded within slope deposits mixed with colluvial loess. the identificati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::1eb1665ce1f9a9c03a2b0bcbff50b44d
http://www.cnr.it/prodotto/i/372964
http://www.cnr.it/prodotto/i/372964
Autor:
Bini M.[1, 2] Zanchetta G.[1, 2] Ribolini A.[1], Salvatore M.C.[1, 3] Baroni C.[1, Pappalardo M.[1], Isola I.[2], Isla F.I.[4] Fucks E.[5], Boretto G.[6] Morigi C.[1, Ragaini L.[1], Marzaioli F.[8], Passariello I.[8]
Publikováno v:
Geografia fisica e dinamica quaternaria (Testo stamp.) 40 (2017): 29–39. doi:10.4461/GFDQ2017.40.3
info:cnr-pdr/source/autori:Bini M.[1,2] Zanchetta G.[1,2] Ribolini A.[1], Salvatore M.C.[1,3] Baroni C.[1,3], Pappalardo M.[1], Isola I.[2], Isla F.I.[4] Fucks E.[5], Boretto G.[6] Morigi C.[1,7], Ragaini L.[1], Marzaioli F.[8], Passariello I.[8]/titolo:Last Interglacial Sea-level highstand deduced from notches and inner margins of marine terraces at Puerto Deseado, Santa Cruz Province, Argentina/doi:10.4461%2FGFDQ2017.40.3/rivista:Geografia fisica e dinamica quaternaria (Testo stamp.)/anno:2017/pagina_da:29/pagina_a:39/intervallo_pagine:29–39/volume:40
info:cnr-pdr/source/autori:Bini M.[1,2] Zanchetta G.[1,2] Ribolini A.[1], Salvatore M.C.[1,3] Baroni C.[1,3], Pappalardo M.[1], Isola I.[2], Isla F.I.[4] Fucks E.[5], Boretto G.[6] Morigi C.[1,7], Ragaini L.[1], Marzaioli F.[8], Passariello I.[8]/titolo:Last Interglacial Sea-level highstand deduced from notches and inner margins of marine terraces at Puerto Deseado, Santa Cruz Province, Argentina/doi:10.4461%2FGFDQ2017.40.3/rivista:Geografia fisica e dinamica quaternaria (Testo stamp.)/anno:2017/pagina_da:29/pagina_a:39/intervallo_pagine:29–39/volume:40
A detailed geomorphological survey was undertaken in the area of Puerto Deseado (Santa Cruz Province, Argentina) to reconstruct the Relative Sea-level (RSL) position during the Last Interglacial highstand. The presence of active and well-preserved ab
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::6a6a6150444174a5c3403e7fac9d25fd
Autor:
Baroni C.[1, Pieruccini P.[3], Bini M.[1], Coltorti M.[3], Fantozzi P.L.[3], Guidobaldi G.[1], Nannini D.[1], Ribolini A.[1], Salvatore M.C.[1]
Publikováno v:
Geografia fisica e dinamica quaternaria (Testo stamp.) 38 (2015): 201–227. doi:10.4461/GFDQ.2015.38.17
info:cnr-pdr/source/autori:Baroni C.[1,2], Pieruccini P.[3], Bini M.[1], Coltorti M.[3], Fantozzi P.L.[3], Guidobaldi G.[1], Nannini D.[1], Ribolini A.[1], Salvatore M.C.[1]/titolo:Geomorphological and neotectonic map of the Apuan Alps (Tuscany, Italy)/doi:10.4461%2FGFDQ.2015.38.17/rivista:Geografia fisica e dinamica quaternaria (Testo stamp.)/anno:2015/pagina_da:201/pagina_a:227/intervallo_pagine:201–227/volume:38
info:cnr-pdr/source/autori:Baroni C.[1,2], Pieruccini P.[3], Bini M.[1], Coltorti M.[3], Fantozzi P.L.[3], Guidobaldi G.[1], Nannini D.[1], Ribolini A.[1], Salvatore M.C.[1]/titolo:Geomorphological and neotectonic map of the Apuan Alps (Tuscany, Italy)/doi:10.4461%2FGFDQ.2015.38.17/rivista:Geografia fisica e dinamica quaternaria (Testo stamp.)/anno:2015/pagina_da:201/pagina_a:227/intervallo_pagine:201–227/volume:38
Renowned since the Roman Period for the extraction of precious marble, the Apuan Alps (northern Tuscany) are an extraordinary region of natural and cultural heritage in the Mediterranean basin and contain a large number of geosites of international a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::d60d229111e7f7f51597bae906072b31
Autor:
Bini M.[1], Isola I.[2], Pappalardo M.[1], Ribolini A.[1] Favalli M.[2] Ragaini L.[1] Zanchetta G. [1, 2
Publikováno v:
Earth surface processes and landforms
39 (2014): 1550–1558. doi:10.1002/esp.3612
info:cnr-pdr/source/autori:Bini M.[1], Isola I.[2], Pappalardo M.[1], Ribolini A.[1] Favalli M.[2] Ragaini L.[1] Zanchetta G. [1,2,3]/titolo:Abrasive notches along the Atlantic Patagonian coast and their potential use as sea level markers: the case of Puerto Deseado (Santa Cruz, Argentina)./doi:10.1002%2Fesp.3612/rivista:Earth surface processes and landforms (Print)/anno:2014/pagina_da:1550/pagina_a:1558/intervallo_pagine:1550–1558/volume:39
39 (2014): 1550–1558. doi:10.1002/esp.3612
info:cnr-pdr/source/autori:Bini M.[1], Isola I.[2], Pappalardo M.[1], Ribolini A.[1] Favalli M.[2] Ragaini L.[1] Zanchetta G. [1,2,3]/titolo:Abrasive notches along the Atlantic Patagonian coast and their potential use as sea level markers: the case of Puerto Deseado (Santa Cruz, Argentina)./doi:10.1002%2Fesp.3612/rivista:Earth surface processes and landforms (Print)/anno:2014/pagina_da:1550/pagina_a:1558/intervallo_pagine:1550–1558/volume:39
Patagonia Argentina is a key area for the study of sea level changes in the southern hemisphere, but the availability of reliable sea level markers in this area is still problematic. In fact the storm deposits (beach ridge) commonly used here to reco
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::6f2e93b03fec33fcaeae9f37227da1e9
Autor:
Zanchetta G.[1, 2, Bini M.[1], Isola I.[2], Pappalardo M.[1], Ribolini A.[1], Consoloni I.[1], Boretto G.[4], Fucks E.[1], Ragaini L.[1], Terrasi F. [6]
Publikováno v:
Holocene (Sevenoaks) 24 (2014): 307–317. doi:10.1177/0959683613518589
info:cnr-pdr/source/autori:Zanchetta G.[1,2,3], Bini M.[1], Isola I.[2], Pappalardo M.[1], Ribolini A.[1], Consoloni I.[1], Boretto G.[4], Fucks E.[1], Ragaini L.[1], Terrasi F. [6]/titolo:Middle-to late-Holocene relative sea-level changes at Puerto Deseado (Patagonia, Argentina)./doi:10.1177%2F0959683613518589/rivista:Holocene (Sevenoaks)/anno:2014/pagina_da:307/pagina_a:317/intervallo_pagine:307–317/volume:24
CIC Digital (CICBA)
Comisión de Investigaciones Científicas de la Provincia de Buenos Aires
instacron:CICBA
info:cnr-pdr/source/autori:Zanchetta G.[1,2,3], Bini M.[1], Isola I.[2], Pappalardo M.[1], Ribolini A.[1], Consoloni I.[1], Boretto G.[4], Fucks E.[1], Ragaini L.[1], Terrasi F. [6]/titolo:Middle-to late-Holocene relative sea-level changes at Puerto Deseado (Patagonia, Argentina)./doi:10.1177%2F0959683613518589/rivista:Holocene (Sevenoaks)/anno:2014/pagina_da:307/pagina_a:317/intervallo_pagine:307–317/volume:24
CIC Digital (CICBA)
Comisión de Investigaciones Científicas de la Provincia de Buenos Aires
instacron:CICBA
Stratigraphic, morphologic and radiocarbon data from Puerto Deseado coastal area (Santa Cruz Province, Argentina) indicate that the Holocene coastline formed in response to the discontinuous aggradation of coarse gravely beaches since c. 6300 cal. yr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e107a4979d5528711af72fcad35a459b
Autor:
Zanchetta G. [1, 2, 5], Consoloni I. [1], Isola I. [2], Pappalardo M. [1], Ribolini A. [1], Aguirre M. [3, 4], Fucks E. [4], Baneschi I. [5], Bini M. [1], Ragaini L.[1], Terrasi F. [6], Boretto G. [7]
Publikováno v:
CIC Digital (CICBA)
Comisión de Investigaciones Científicas de la Provincia de Buenos Aires
instacron:CICBA
Italian Journal of Geosciences (Online) 131 (2012): 19–31.
info:cnr-pdr/source/autori:Zanchetta G. [1, 2, 5]; Consoloni I. [1]; Isola I. [2]; Pappalardo M. [1]; Ribolini A. [1]; Aguirre M. [3, 4]; Fucks E. [4]; Baneschi I. [5]; Bini M. [1]; Ragaini L.[1]; Terrasi F. [6]; Boretto G. [7]/titolo:New insights on the Holocene marine transgression in the Bahia Camarones (Chubut, Argentina)./doi:/rivista:Italian Journal of Geosciences (Online)/anno:2012/pagina_da:19/pagina_a:31/intervallo_pagine:19–31/volume:131
Comisión de Investigaciones Científicas de la Provincia de Buenos Aires
instacron:CICBA
Italian Journal of Geosciences (Online) 131 (2012): 19–31.
info:cnr-pdr/source/autori:Zanchetta G. [1, 2, 5]; Consoloni I. [1]; Isola I. [2]; Pappalardo M. [1]; Ribolini A. [1]; Aguirre M. [3, 4]; Fucks E. [4]; Baneschi I. [5]; Bini M. [1]; Ragaini L.[1]; Terrasi F. [6]; Boretto G. [7]/titolo:New insights on the Holocene marine transgression in the Bahia Camarones (Chubut, Argentina)./doi:/rivista:Italian Journal of Geosciences (Online)/anno:2012/pagina_da:19/pagina_a:31/intervallo_pagine:19–31/volume:131
The stratigraphic reconstruction of the northern sector of the Bahía Camarones (Chubut, Argentina) allowed to improve our understanding of the Holocene marine transgression in the area. The first phase of the maximum of the transgression, is interpr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::795723a73643c1944d1a76e8fc83458d
http://hdl.handle.net/11591/188182
http://hdl.handle.net/11591/188182
Autor:
Consoloni I.[1], Zanchetta G.[1, 3, Aguirre M.[2], Baneschi I.[3], Bini M.[1], Boretto G.M.[2], Dallai L. [3], D'Orazio M.[1], Fallick A.E[4], Guidi M.[3], Hellstrom J.C.[5], Isola I.[6], Fucks E.[2], Mazzarini F.[6], Pappalardo M. [1], Ribolini A. [1]
Publikováno v:
Il Quaternario italiano: conoscenze e prospettive, Roma, 24-25 Febbraio
info:cnr-pdr/source/autori:Consoloni I.[1], Zanchetta G.[1,3,6], Aguirre M.[2], Baneschi I.[3], Bini M.[1], Boretto G.M.[2], Dallai L. [3], D'Orazio M.[1], Fallick A.E[4], Guidi M.[3], Hellstrom J.C.[5], Isola I.[6], Fucks E.[2], Mazzarini F.[6], Pappalardo M. [1], Ribolini A. [1]/congresso_nome:Il Quaternario italiano: conoscenze e prospettive/congresso_luogo:Roma/congresso_data:24-25 Febbraio/anno:2011/pagina_da:/pagina_a:/intervallo_pagine
info:cnr-pdr/source/autori:Consoloni I.[1], Zanchetta G.[1,3,6], Aguirre M.[2], Baneschi I.[3], Bini M.[1], Boretto G.M.[2], Dallai L. [3], D'Orazio M.[1], Fallick A.E[4], Guidi M.[3], Hellstrom J.C.[5], Isola I.[6], Fucks E.[2], Mazzarini F.[6], Pappalardo M. [1], Ribolini A. [1]/congresso_nome:Il Quaternario italiano: conoscenze e prospettive/congresso_luogo:Roma/congresso_data:24-25 Febbraio/anno:2011/pagina_da:/pagina_a:/intervallo_pagine
The selection of suitable samples is a fundamental target in order to obtain reliable results in the field of radiometric dating and paleoclimate. Marine molluscs are particularly interesting in this respect in what different radiometric methods (e.g
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::135e023803c08b58c39c1db15ac34f01
http://www.cnr.it/prodotto/i/302470
http://www.cnr.it/prodotto/i/302470