Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Renzo, Valloni"'
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 105, Iss 1 (1999)
Below the Monte Cassio helminthoid Flysch of the type locality, a well exposed basal complex outcrops in which Cenomanian turbidites of up to 200 m thickness are recognized. The bulk of these turbidites, named here Case Baruzzo Sandstone (CBS), consi
Externí odkaz:
https://doaj.org/article/cce6cb86c5e44e01a27da3f90de050f1
Publikováno v:
Journal of Coastal Research. 61:1-7
BARSANTI, M., CALDA, N and VALLONI, R., 2011. The Italian Coasts: a Natural Laboratory for the Quality Evaluation of Beach Replenishments. In: Micallef, A. (ed.), MCRR3-2010 Conference Proceedings, Journal of Coastal Research, Special Issue, No. 61,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7fc5ab4e0a35190450539baf67d3c540
https://doi.org/10.2112/si61-001.1
https://doi.org/10.2112/si61-001.1
Autor:
Renzo Valloni
Publikováno v:
Quaternary International. :510
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ef67bff50844419b93af854612044355
https://doi.org/10.1016/j.quaint.2012.08.1757
https://doi.org/10.1016/j.quaint.2012.08.1757
Autor:
G. Mezzadri, Renzo Valloni
Publikováno v:
Sedimentology. 31:353-364
The compositional variability shown by sands of present continental margins was determined through conventional microscopic techniques. This allowed the establishment of a descriptive classification of deep-sea terrigenous sands based on a restricted
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ed1fb9a07ba58cde4ff8e54c54c14421
https://doi.org/10.1111/j.1365-3091.1984.tb00864.x
https://doi.org/10.1111/j.1365-3091.1984.tb00864.x
Publikováno v:
Geological Society, London, Special Publications. 10:551-561
SUMMARY: Petrographic and chemical examination of modern deep-sea sands shows a clear distinction between active and passive plate-tectonic settings. Among active settings, sands from forearc basins of island arcs and basins from strike-slip continen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4c193dc61fd9975e3923280512f869e1
https://doi.org/10.1144/gsl.sp.1982.010.01.36
https://doi.org/10.1144/gsl.sp.1982.010.01.36
Autor:
Renzo Valloni, J. Barry Maynard
Publikováno v:
Deep-Water Turbidite Systems
Complete petrographic analyses of modern deep-sea sands are surprisingly rare, but are needed if problems such as the influence of tectonics on petrology, or changes in petrology due to diagenesis, are to be understood in ancient sandstones. This pap
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::beba1f21424c1c230c18681c208d9ef0
https://doi.org/10.1111/j.1365-3091.1981.tb01664.x
https://doi.org/10.1111/j.1365-3091.1981.tb01664.x
Autor:
Renzo Valloni
Publikováno v:
Provenance of Arenites ISBN: 9789048184132
Data concerning the composition of sands from modern continental margins has enabled an actualistic scheme of provenances to be formulated. In order to avoid secondary controls of detrital modes some of the variables have been standardized. This mean
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2c96628ee39087ed7340fe1b8fa0e837
https://doi.org/10.1007/978-94-017-2809-6_14
https://doi.org/10.1007/978-94-017-2809-6_14
The aquifer is located on the coastal sand dune that was deposited during the marine transgression that took place about 5000-6000 years ago: the marine trasgression reached inland as much as from 2 to 1 Km, from north to south. A marsh area develope
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4094::528940b64d86b72c937a009e48dab7a7
http://hdl.handle.net/11585/66360
http://hdl.handle.net/11585/66360