Zobrazeno 1 - 6 of 6 pro vyhledávání: '"Giaccio B. 1"'
1
Duration and dynamics of the best orbital analogue to the present interglacial
Autor: Giaccio B.[1], Regattieri E.[1, 2, Zanchetta G.[1, Nomade S.[4], Renne P.R.[5, Sprain C.J.[5, Drysdale R.N.[7, Tzedakis P.C.[9], Messina P.[1], Scardia G.[1, 10], Sposato A.[1], Bassinot F.[4]
Publikováno v: Geology
Geology, 2015, 43 (7), pp.603-606. ⟨10.1130/G36677.1⟩
Geology, Geological Society of America, 2015, 43 (7), pp.603-606. ⟨10.1130/G36677.1⟩
Geology, vol 43, iss 7
Geology (Boulder Colo.) 43 (2015): 603–606. doi:10.1130/G36677.1
info:cnr-pdr/source/autori:Giaccio B.[1], Regattieri E.[1,2,3], Zanchetta G.[1,2,3], Nomade S.[4], Renne P.R.[5,6], Sprain C.J.[5,6], Drysdale R.N.[7,8], Tzedakis P.C.[9], Messina P.[1], Scardia G.[1,10], Sposato A.[1], Bassinot F.[4]/titolo:Duration and dynamics of the best orbital analogue to the present interglacial/doi:10.1130%2FG36677.1/rivista:Geology (Boulder Colo.)/anno:2015/pagina_da:603/pagina_a:606/intervallo_pagine:603–606/volume:43
Past orbital analogues to the current interglacial, such as Marine Isotope Stage 19c (MIS 19c, ca. 800 ka), can provide reliable reference intervals for evaluating the timing and the duration of the Holocene and factors inherent in its climatic progr
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::02fc8c1f8aa8ef7e9dd21490f5637b40
https://doi.org/10.1130/g36677.1
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2
Environmental variability between the penultimate deglaciation and the mid Eemian: Insights from Tana che Urla (central Italy) speleothem trace element record
Autor: Regattieri E.[1, Zanchetta G.[2, 3, 4] Drysdale R.N.[5, Isola I.[4], Woodhead J.D.[7], Hellstrom J.C.[7], Giaccio B.[1], Greig A.[7], Baneschi I.[3], Dotsika E. [8]
Publikováno v: Quaternary Science Reviews
Quaternary Science Reviews, Elsevier, 2016, 152, pp.80-92
Quaternary science reviews 152 (2016): 80–92. doi:10.1016/j.quascirev.2016.09.027
info:cnr-pdr/source/autori:Regattieri E.[1,3], Zanchetta G.[2,3,4] Drysdale R.N.[5,6], Isola I.[4], Woodhead J.D.[7], Hellstrom J.C.[7], Giaccio B.[1], Greig A.[7], Baneschi I.[3], Dotsika E. [8]/titolo:Environmental variability between the penultimate deglaciation and the mid Eemian: Insights from Tana che Urla (central Italy) speleothem trace element record/doi:10.1016%2Fj.quascirev.2016.09.027/rivista:Quaternary science reviews/anno:2016/pagina_da:80/pagina_a:92/intervallo_pagine:80–92/volume:152
International audience; A trace element record (Mg, Sr, Ba, Al, Si, P, Y, Zn) covering the ca. 133 ka to ca. 124 ka time interval was acquired from a flowstone core from Tana che Urla Cave (central Italy). It was compared with stable isotope data to
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6a6f6b6e59a13e714f40e963d590b725
https://hal.archives-ouvertes.fr/hal-02009232
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3
Paleoseismologic and geomorphic constraints to the deformation style and activity of the Cittanova Fault (southern Calabria, Italy)
Autor: Peronace E. 12, Della Seta M. 2, Fredi P. 2, Galli P. 13, Giaccio B. 1, Messina P. 1, Troiani F. 2
Publikováno v: EGU General Assembly 2016, Vienna, 2016
info:cnr-pdr/source/autori:Peronace E. 12, Della Seta M. 2, Fredi P. 2, Galli P. 13, Giaccio B. 1, Messina P. 1, Troiani F. 2/congresso_nome:EGU General Assembly 2016/congresso_luogo:Vienna/congresso_data:2016/anno:2016/pagina_da:/pagina_a:/intervallo_pagine
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::fa5516e982da88a8fa85520aa3e3a5bb
http://www.cnr.it/prodotto/i/411672
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4
Integrazione di analisi geo-morfometriche e paleosismologiche per la definizione dell'attività della faglia di Cittanova (Calabria meridionale)
Autor: Peronace E. 1, 2, Della Seta M. 2, Troiani F. 2, Galli P. 1, 3, Giaccio B. 1, Messina P. 1, Fredi P. 2
Publikováno v: 35° Convegno Nazionale GNGTS, pp. 170–174, Lecce, 22-24 Novembre 2016
info:cnr-pdr/source/autori:Peronace E. 1,2, Della Seta M. 2, Troiani F. 2, Galli P. 1,3, Giaccio B. 1, Messina P. 1, Fredi P. 2/congresso_nome:35° Convegno Nazionale GNGTS/congresso_luogo:Lecce/congresso_data:22-24 Novembre 2016/anno:2016/pagina_da:170/pagina_a:174/intervallo_pagine:170–174
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::7f2d6a7e678b132c044981dc8d8669e4
https://publications.cnr.it/doc/411701
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6
The late MIS 5 Mediterranean tephra markers: a reappraisal from peninsular Italy terrestrial records
Autor: Giaccio B.[1], Nomade S.[2], Wulf S.[3], Isaia R.[4], Sottili G.[1], Cavuoto G.[1], Galli P.[1, Messina P.[1], Sposato A.[1], Sulpizio R.[6, Zanchetta G.[8, 9, 10]
Publikováno v: Quaternary Science Reviews
Quaternary Science Reviews, 2012, 56, pp.31-45. ⟨10.1016/j.quascirev.2012.09.009⟩
Quaternary science reviews 56 (2012): 31–45. doi:10.1016/j.quascirev.2012.09.009
info:cnr-pdr/source/autori:Giaccio B., Nomade S., Wulf S., Isaia R., Sottili G., Cavuoto G., Galli P., Messina P., Sposato A., Sulpizio R., Zanchetta G/titolo:The late MIS 5 Mediterranean tephra markers: a reappraisal from peninsular Italy terrestrial records/doi:10.1016%2Fj.quascirev.2012.09.009/rivista:Quaternary science reviews/anno:2012/pagina_da:31/pagina_a:45/intervallo_pagine:31–45/volume:56
Quaternary Science Reviews, Elsevier, 2012, 56, pp.31-45. ⟨10.1016/j.quascirev.2012.09.009⟩
info:cnr-pdr/source/autori:Giaccio B.[1], Nomade S.[2], Wulf S.[3], Isaia R.[4], Sottili G.[1], Cavuoto G.[1], Galli P.[1,5], Messina P.[1], Sposato A.[1], Sulpizio R.[6,7], Zanchetta G.[8,9,10]/titolo:The late MIS 5 Mediterranean tephra markers: a reappraisal from peninsular Italy terrestrial records/doi:10.1016%2Fj.quascirev.2012.09.009/rivista:Quaternary science reviews/anno:2012/pagina_da:31/pagina_a:45/intervallo_pagine:31–45/volume:56
We present new tephrostratigraphic records from the late MIS 5 (ca 110–80 ka) terrestrial sediments from southern and central Italy. On the one hand, the central Italy record consists of an outcropping lacustrine sequence from the Sulmona intermoun
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::970bd3766418d26e531595aba5b61bfe
https://hal.science/hal-03205580
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