Výsledky vyhledávání - "Catanzariti R.(3)"

The western Durkan Complex (Makran Accretionary Prism, SE Iran): A Late Cretaceous tectonically disrupted seamounts chain and its role in controlling deformation style

Autor: Barbero E.[1], Pandolfi L.[2, Delavari M.[4], Dolati A.[4], Saccani E.[1], Catanzariti R.[3], Luciani V.[1], Chiari M.[5], Marroni M.[2

Publikováno v: Geoscience Frontiers, Vol 12, Iss 3, Pp 101106-(2021)
Geosciences Frontiers 12 (2021): 1–25. doi:10.1016/j.gsf.2020.12.001
info:cnr-pdr/source/autori:Barbero E.[1], Pandolfi L.[2,3], Delavari M.[4], Dolati A.[4], Saccani E.[1], Catanzariti R.[3], Luciani V.[1], Chiari M.[5], Marroni M.[2,3]/titolo:The western Durkan Complex (Makran Accretionary Prism, SE Iran): A Late Cretaceous tectonically disrupted seamounts chain and its role in controlling deformation style/doi:10.1016%2Fj.gsf.2020.12.001/rivista:Geosciences Frontiers/anno:2021/pagina_da:1/pagina_a:25/intervallo_pagine:1–25/volume:12

The Durkan Complex is a key tectonic element of the Makran accretionary prism (SE Iran) and it has been interpreted as representing a continental margin succession. We present here a multidisciplinary study of the western Durkan Complex, which is bas

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ed0402df3079bdb32551b0bd7a827287
http://hdl.handle.net/11392/2431976

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Carbon cycle instability and orbital forcing during the Middle Eocene Climatic Optimum

Autor: Giorgioni M.[1, Jovane L.[1], Rego E.[1, Rodelli D.[1], Frontalini F.[2], Coccioni R.[2], Catanzariti R.[3], Özcan E[4]

Publikováno v: Scientific reports (Nature Publishing Group) 9 (2019). doi:10.1038/s41598-019-45763-2
info:cnr-pdr/source/autori:Giorgioni M.[1,5], Jovane L.[1], Rego E.[1,6], Rodelli D.[1], Frontalini F.[2], Coccioni R.[2], Catanzariti R.[3], Özcan E[4]/titolo:Carbon cycle instability and orbital forcing during the Middle Eocene Climatic Optimum/doi:10.1038%2Fs41598-019-45763-2/rivista:Scientific reports (Nature Publishing Group)/anno:2019/pagina_da:/pagina_a:/intervallo_pagine:/volume:9
Scientific Reports, Vol 9, Iss 1, Pp 1-10 (2019)
Scientific Reports
Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual)
Universidade de São Paulo (USP)
instacron:USP

The Middle Eocene Climatic Optimum (MECO) is a global warming event that occurred at about 40 Ma. In comparison to the most known global warming events of the Paleogene, the MECO has some peculiar features that make its interpretation controversial.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ab59544bfadac9d721e4192a3551aca3

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Fossil whale barnacles from the lower Pleistocene of Sicily shed light on the coeval Mediterranean cetacean fauna

Autor: Collareta A.[1], Insacco G.[2], Reitano A.[2], Catanzariti R.[3], Bosselaers M.[4], Montes M.[5], Bianucci G.[1]

Publikováno v: Carnets de géologie (2018): 9–22.
info:cnr-pdr/source/autori:Collareta A.[1], Insacco G.[2], Reitano A.[2], Catanzariti R.[3], Bosselaers M.[4], Montes M.[5], Bianucci G.[1]/titolo:Fossil whale barnacles from the lower Pleistocene of Sicily shed light on the coeval Mediterranean cetacean fauna/doi:/rivista:Carnets de géologie/anno:2018/pagina_da:9/pagina_a:22/intervallo_pagine:9–22/volume

We report on three shells of whale barnacle (Cirripedia: Coronulidae) collected from Pleistocene shallow-marine deposits exposed at Cinisi (northwestern Sicily, southern Italy). These specimens are identified as belonging to the extinct species Coron

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::cb2f6d9c65ca9cdc1034865c9c1f1aec
https://publications.cnr.it/doc/386480

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The Boeotian Flysch revisited: new constraints on ophiolite obduction in central Greece

Autor: Nirta G.(1), Moratti G.(2), Piccardi L.(2), Montanari D.(2), Catanzariti R.(3), Carras N.(4), Papini M.(1)

Publikováno v: Ofioliti (Bologna) 40 (2015): 107–123. doi:10.4454/ofioliti.v40i2.438
info:cnr-pdr/source/autori:Nirta G.(1); Moratti G.(2); Piccardi L.(2); Montanari D.(2); Catanzariti R.(3); Carras N.(4); Papini M.(1)/titolo:The Boeotian Flysch revisited: new constraints on ophiolite obduction in central Greece/doi:10.4454%2Fofioliti.v40i2.438/rivista:Ofioliti (Bologna)/anno:2015/pagina_da:107/pagina_a:123/intervallo_pagine:107–123/volume:40

This paper reports new data on biostratigraphy, stratigraphy and syn-sedimentary deformation of the so-called "Boeotian Flysch" cropping out in key areas in Central Greece (Levadhia, Parnassus, Iti). Because of its age, sedimentary evolution and mech

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::117c787e7e029b223e7b07e6197ad1ad

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Updated picture of the Ligurian and Sub-Ligurian units in the Mt. Amiata area (Tuscany, Italy): elements for their correlation in the framework of the Northern Apennines

Autor: Marroni M.[1, Pandeli E.[2, Pandolfi L.[1, Catanzariti R.[3]

Publikováno v: Italian Journal of Geosciences (Online) 134 (2015): 200–218. doi:10.3301/IJG.2014.47
info:cnr-pdr/source/autori:Marroni M.[1,3], Pandeli E.[2,4], Pandolfi L.[1,3], Catanzariti R.[3]/titolo:Updated picture of the Ligurian and Sub-Ligurian units in the Mt. Amiata area (Tuscany, Italy): elements for their correlation in the framework of the Northern Apennines/doi:10.3301%2FIJG.2014.47/rivista:Italian Journal of Geosciences (Online)/anno:2015/pagina_da:200/pagina_a:218/intervallo_pagine:200–218/volume:134

The Mt. Amiata region (Southern Tuscany, Italy) represents the southernmost area of the Northern Apennines in which different lithologies belonging to the Ligurian and Sub-Ligurian units crop out widely. This paper provides an update on the stratigra

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::15ca3e57687363333ca7839f236992f2
https://publications.cnr.it/doc/332099

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Unravelling basin shoulder dynamics through detrital apatite fission-track signature: the case of the Quaternary Mugello Basin, Italy

Autor: Maria Laura Balestrieri, Rita Catanzariti, Marco Benvenuti

Publikováno v: Geological magazine (Online) (2017). doi:10.1017/S0016756817000073
info:cnr-pdr/source/autori:Balestrieri M.L.[1], Benvenuti M.[2], Catanzariti R.[3]/titolo:Unravelling basin shoulder dynamics through detrital apatite fission-track signature: the case of quaternary Mugello basin, Italy./doi:10.1017%2FS0016756817000073/rivista:Geological magazine (Online)/anno:2017/pagina_da:/pagina_a:/intervallo_pagine:/volume

Detrital apatite fission-track (AFT) thermochronology has been applied to lower Pleistocene lacustrine fan-delta sediments of the NE shoulder of the Mugello Basin, the youngest and closest to the main watershed among the Northern Apennines intermonta

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0255c23b62c4dc864b90dd818515819c
https://doi.org/10.1017/s0016756817000073

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Mid-eocene giant slope failure (Sedimentary mélanges) in the ligurian accretionary wedge (nw italy) and relationships with tectonics, global climate change and the dissociation of gas hydrates

Autor: Gian Andrea Pini, Andrea Festa, Rita Catanzariti, Simona Cavagna, Edoardo Barbero

Publikováno v: Journal of the Geological Society (Online) (2019).
info:cnr-pdr/source/autori:Festa A.[1], Cavagna S.[1], Barbero E.[2], Catanzariti R.[3], Pini A.[4]/titolo:Mid-Eocene giant slope failure (sedimentary mélanges) in the Ligurian accretionary wedge (NW Italy) and relationships with tectonics, global climate change and the dissociation of gas hydrates./doi:/rivista:Journal of the Geological Society (Online)/anno:2019/pagina_da:/pagina_a:/intervallo_pagine:/volume

Upper Lutetian-Bartonian sedimentary mélanges, corresponding to ancient mud-rich submarine mass transport deposits, are widely distributed over an area c. 300 km long and tens of kilometres wide along the exhumed outer part of the External Ligurian

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::631bdcc1e4ecd9779f4474a75ecf8c6d
http://hdl.handle.net/11368/2969473

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Redefinition of the Ligurian Units at the Alps-Apennines junction (NW Italy) and their role in the evolution of the Ligurian accretionary wedge: constraints from mélanges and broken formations

Autor: Edoardo Barbero, Roberta D'Onofrio, Emilio Saccani, Andrea Festa, Rita Catanzariti

Publikováno v: Journal of the Geological Society (Lond.) (2019). doi:10.1144/jgs2019-022
info:cnr-pdr/source/autori:Barbero E.[1], Festa A.[2], Saccani E.[1], Catanzariti R.[3], D'Onofrio R.[1]/titolo:Redefinition of the Ligurian Units at the Alps-Apennines junction (NW Italy) and their role in the evolution of the Ligurian accretionary wedge: constraints from mélanges and broken formations./doi:10.1144%2Fjgs2019-022/rivista:Journal of the Geological Society (Lond.)/anno:2019/pagina_da:/pagina_a:/intervallo_pagine:/volume

We document that the undifferentiated chaotic Ligurian Units of the Monferrato–Torino Hill sector (MO-TH) at the Alps–Apennines junction consist of three different units that are comparable with the Cassio, Caio and Sporno Units of the External L

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f9aaa49e22bc0254b7aab13548745758
https://jgs.lyellcollection.org/

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Biozonation and biochronology of Paleogene calcareous nannofossils from low and middle latitudes

Autor: Claudia Agnini, Jan Backman, Heiko Pälike, Domenico Rio, Rita Catanzariti, Eliana Fornaciari, Isabella Raffi

Publikováno v: Newsletters on stratigraphy 47 (2014): 131–181. doi:10.1127/0078-0421/2014/0042
info:cnr-pdr/source/autori:Agnini C.[1], Fornaciari E.[1], Raffi I.[2], Catanzariti R.[3], Heiko P. [4], Backman J.[5], Rio D. [1]/titolo:Biozonation and biochronology of Paleogene calcareous nannofossils from low and middle latitudes./doi:10.1127%2F0078-0421%2F2014%2F0042/rivista:Newsletters on stratigraphy/anno:2014/pagina_da:131/pagina_a:181/intervallo_pagine:131–181/volume:47

Calcareous nannofossils have provided a powerful biostratigraphic tool since the 1950's and 1960's, when several milestone papers began to highlight their potential use in dating Cenozoic sediments and rocks. Here, we present a new calcareous nannofo

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::22e15ca45f9661bbeb8a3720c81a523b
https://doi.org/10.1127/0078-0421/2014/0042

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Systematics, biostratigraphy and evolutionary pattern of the Oligo-Miocene marine mammals from the Maltese Islands

Autor: Silvia Sorbi, Giovanni Bianucci, Charles G. Bonavia, Rita Catanzariti, Richard Curmi, Michael Gatt, Angelo Varola

Publikováno v: GEOBIOS 44 (2011): 549–585. doi:10.1016/j.geobios.2011.02.009
info:cnr-pdr/source/autori:Bianucci, G. [ 1 ] ; Gatt, M. [ 2 ] ; Catanzariti, R. [ 3 ] ; Sorbi, S. [ 4 ] ; Bonavia, C. G. [ 5 ] ; Curmi, R. [ 6 ] ; Varola, A. [7]/titolo:Systematics, biostratigraphy and evolutionary pattern of the oligo-miocene marine mammals from the Maltese islands/doi:10.1016%2Fj.geobios.2011.02.009/rivista:GEOBIOS/anno:2011/pagina_da:549/pagina_a:585/intervallo_pagine:549–585/volume:44

An overview of the upper Oligocene-upper Miocene marine sediments outcropping in the Maltese Islands provides a detailed stratigraphical setting of several marine mammal assemblages. The studied fossil material collected within the entire sequence, i

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b1d360a1fe3538683da9eeb12f0aa88f
https://doi.org/10.1016/j.geobios.2011.02.009

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