Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/9152
DC Field | Value | Language |
---|---|---|
dc.contributor.authorall | Saroli, M.; Università degli Studi di Cassino e del Lazio Meridionale | en |
dc.contributor.authorall | Lancia, M.; Università degli Studi di Cassino e del Lazio Meridionale | en |
dc.contributor.authorall | Albano, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italia | en |
dc.contributor.authorall | Modoni, G.; Università degli Studi di Cassino e del Lazio Meridionale | en |
dc.contributor.authorall | Moro, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italia | en |
dc.contributor.authorall | Scarascia Mugnozza, G.; Sapienza Università di Roma | en |
dc.date.accessioned | 2014-11-17T14:34:24Z | en |
dc.date.available | 2014-11-17T14:34:24Z | en |
dc.date.issued | 2014-10 | en |
dc.identifier.uri | http://hdl.handle.net/2122/9152 | en |
dc.description.abstract | This paper presents the outcome of photogeological analysis, field survey as well as borehole correlation, to add new data concerning the intermontane Cassino basin and define facies and thickness of its Quaternary deposits. The investigated area is located in the end sector of the Latina Valley, Southern Lazio and belongs to the Lazio–Abruzzi domain. With a maximum extension of 250 km2 and a NW–SE trend, this paleo-lake was created by lava flows from the Roccamonfina volcano, which barred the Latina Valley. The lacustrine facies were described during the 1960s but available bibliographic data about its spatial distribution and its relationship with the Mesozoic– Cenozoic bedrock are scarce. The thickness of Quaternary deposits has been deeply influenced by inherited paleomorphologies. Indeed the geological reconstruction of the basin has outlined the presence of an underlying horst and graben structure. This latter obscured the contractional tectonics originated by the orogenetic deformation, even if new structures have been recognized at the foot of Montecassino Hill. We infer that a key role has been per- formed by the Roveto Valley–Atina–Caserta fault, between Atina and San Pietro Infine. | en |
dc.language.iso | English | en |
dc.publisher.name | Springer Milan | en |
dc.relation.ispartof | Rendiconti Lincei. Scienze Fisiche e Naturali (Springer) | en |
dc.relation.ispartofseries | 2 SUPP/ 25 (2014) | en |
dc.subject | Central Apennines | en |
dc.subject | Quaternary basin | en |
dc.subject | Normal faulting | en |
dc.subject | Lacustrine deposits | en |
dc.title | New geological data on the Cassino intermontane basin, central Apennines, Italy | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.description.pagenumber | 189-196 | en |
dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.03. Geomorphology | en |
dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.08. Sediments: dating, processes, transport | en |
dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.09. Structural geology | en |
dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.10. Stratigraphy | en |
dc.identifier.doi | 10.1007/s12210-014-0338-5 | en |
dc.description.obiettivoSpecifico | 2T. Tettonica attiva | en |
dc.description.journalType | JCR Journal | en |
dc.description.fulltext | restricted | en |
dc.relation.issn | 2037-4631 | en |
dc.relation.eissn | 1720-0776 | en |
dc.contributor.author | Saroli, M. | en |
dc.contributor.author | Lancia, M. | en |
dc.contributor.author | Albano, M. | en |
dc.contributor.author | Modoni, G. | en |
dc.contributor.author | Moro, M. | en |
dc.contributor.author | Scarascia Mugnozza, G. | en |
dc.contributor.department | Università degli Studi di Cassino e del Lazio Meridionale | en |
dc.contributor.department | Università degli Studi di Cassino e del Lazio Meridionale | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia | en |
dc.contributor.department | Università degli Studi di Cassino e del Lazio Meridionale | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia | en |
dc.contributor.department | Sapienza Università di Roma | en |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | restricted | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | University of Cassino | - |
crisitem.author.dept | Università degli Studi di Cassino e del Lazio Meridionale | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia | - |
crisitem.author.dept | Università degli studi di Cassino e del Lazio meridionale | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia | - |
crisitem.author.dept | Dipartimento di Scienze della Terra, Universita` di Roma ‘‘La Sapienza’’ | - |
crisitem.author.orcid | 0000-0001-9499-3960 | - |
crisitem.author.orcid | 0000-0002-8703-6174 | - |
crisitem.author.orcid | 0000-0003-2772-2401 | - |
crisitem.author.orcid | 0000-0002-3408-8034 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
Appears in Collections: | Article published / in press |
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art%3A10.1007%2Fs12210-014-0338-5.pdf | 2.23 MB | Adobe PDF |
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