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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