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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7649
DC FieldValueLanguage
dc.contributor.authorallZanchetta, G.; Dipartimento di Scienze della Terra, Università di Pisa, Pisa, Italyen
dc.contributor.authorallIsola, I.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.authorallPiccini, L.; Dipartimento di Scienze della Terra, Università di Firenze, Firenze Italyen
dc.contributor.authorallDini, A.; Istituto di Geoscienze e Georisorse, CNR Pisaen
dc.date.accessioned2012-01-29T09:53:55Zen
dc.date.available2012-01-29T09:53:55Zen
dc.date.issued2011en
dc.identifier.urihttp://hdl.handle.net/2122/7649en
dc.description.abstractMonte Corchia is one of the most typical geological structure of the Alpi Apuane but this is not the only peculiar aspect of this territory. Within a very small area it is possible to combine structural geology, marble exploitation, geomorphology and ore deposits. The last point is of worth of interest because the area has been the subject of ore exploitation until the recent past. Within the marble succession of the Corchia synclinal core develops the longest Italian cave with 52 km of passages and galleries. Ongoing researches are exploring the huge paleoclimatic archives preserved within the carbonate concretion of the cave and are reconstructing, with extreme detail the climatic and environmental evolution of this sector of the Mediterranean basin.en
dc.language.isoEnglishen
dc.publisher.nameSocietà Geologica Italiana; ISPRAen
dc.relation.ispartofGeological Field Tripsen
dc.relation.ispartofseries2.1/3(2011)en
dc.subjectGeologyen
dc.subjectMineralogyen
dc.subjectPaleoclimateen
dc.subjectApuan Alpsen
dc.titleThe Corchia Cave (Alpi Apuane): a 2 Ma long temporal window on the Earth climateen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber1-55en
dc.identifier.URLhttp://www.isprambiente.it/site/it-IT/Pubblicazioni/Periodici_tecnici/Geological_Field_Tripsen
dc.subject.INGV03. Hydrosphere::03.01. General::03.01.06. Paleoceanography and paleoclimatologyen
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.03. Geomorphologyen
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.05. Mineralogy and petrologyen
dc.identifier.doi10.3301/GFT.2011.02en
dc.description.obiettivoSpecifico3.7. Dinamica del clima e dell'oceanoen
dc.description.journalTypeN/A or not JCRen
dc.description.fulltextopenen
dc.contributor.authorZanchetta, G.en
dc.contributor.authorIsola, I.en
dc.contributor.authorPiccini, L.en
dc.contributor.authorDini, A.en
dc.contributor.departmentDipartimento di Scienze della Terra, Università di Pisa, Pisa, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.departmentDipartimento di Scienze della Terra, Università di Firenze, Firenze Italyen
dc.contributor.departmentIstituto di Geoscienze e Georisorse, CNR Pisaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia-
crisitem.author.orcid0000-0002-3911-4676-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent03. Hydrosphere-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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