Please use this identifier to cite or link to this item: http://dx.doi.org/10.15165/studgeocam-1288
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dc.contributor.authorCALAMITA, F.-
dc.contributor.authorCENTAMORE, E.-
dc.contributor.authorCHIOCCHINI, U.-
dc.contributor.authorDEIANA, G.-
dc.contributor.authorMICARELLI, A.-
dc.contributor.authorPOTETTI, M.-
dc.contributor.authorROMANO, A.-
dc.date.accessioned2017-09-08T08:29:47Z-
dc.date.available2017-09-08T08:29:47Z-
dc.date.issued1979-
dc.identifier.citationStudi geologici camerti, 5, 1979, pp. 67-82 + cartaen_US
dc.identifier.issn0392-0631-
dc.identifier.urihttp://localhost:8080/jspui/handle/1336/65-
dc.description.abstractA strong synsedimentary tectonic phase developed during the Middle Tortonian-Messinian - but already acting since the begin­ning of the Miocene, as showed by the lithologic and thickness dif­ferences occuring within the Bisciaro-Schlier sequence - subdivides the Camerino Basin into two main depressions: the small Collama­to Subbasin, and the Matelica-Fiegni Subbasin. The turbidite depo­sition started during the Middle Tortonian in the deeper parts of the basins while the hemipelagic deposition of the Schlier goes on in the higher areas during the entire Tortonian. The Gessoso-solfifera Formation and the Colombacci Formation dose the Miocene se­quence. [...]en_US
dc.publisherUniversità di Camerinoen_US
dc.subjectAnalisi di Facies - evoluzione tettonico-sedimentaria - Miocene - Bacino di Camerino (Marche)en_US
dc.subjectFacies analysis - tectonic-sedimentary evolution - Camerino basin (Marche)en_US
dc.titleANALISI DELL'EVOLUZIONE TETTONICO-SEDIMENTARIA DEI «BACINI MINORI» TORBIDITICI DEL MIOCENE MEDIO-SUPERIORE NELL'APPENNINO UMBRO-MARCHIGIANO E LAZIALE-ABRUZZESE: 7) IL BACINO DI CAMERINOen_US
dc.description.pages67-82 + carta-
dc.identifier.sequenza4-
Appears in Volumess:Volume 05 (1979)

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