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of 36
pro vyhledávání: '"LUCENTE C. C."'
The town of San Leo, situated in the northern Apennines of Italy, is subject to slope instability phenomena due to its geological/structural setting. The 3D geological model of the eastern sector of the San Leo rocky plateau has been developed throug
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4094::14744a8fa2fecb239ec786a3aa3e29f3
https://hdl.handle.net/11585/861202
https://hdl.handle.net/11585/861202
L’articolo illustra una nuova carta geologica in scala 1/2000 della Rupe di San Leo, che è una spettacolare e delicata forma del rilievo posta al centro della Coltre della Val Marecchia. La Rupe è costituita da una successione epiligure che compr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::a4d1a814afd5ccbd42d87e513c2bb720
http://hdl.handle.net/11585/698699
http://hdl.handle.net/11585/698699
Akademický článek
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In this study we combine observations and analytical data from largescale (10-100s of m-thick and 100 m2-extensive), siliciclastic and carbonate MTD/MTCs belonging to the Oligocene - Miocene foredeep and wedge-top successions of the Northern Apennine
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3730::da43dbc8b11be4f646b721e01b86478f
http://hdl.handle.net/11588/820237
http://hdl.handle.net/11588/820237
Autor:
RIZZINI F., TORELLI L., PASCUCCI V., CAMURRI F., ARTONI A., BERNINI M., LUCENTE C. C., MANZI V., PALTRINIERI W., PAPANI G., ROVERI M., PINI, GIAN ANDREA
A geological transect from the abyssal plain of the Ligurian Sea to the Po Plain, realised integrating seismic profiles (ENI, BG Group and CROP data set), well data and surface geology, is presented and discussed in order to highlight Messinian depos
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::d76b0c4e8e9027277edae97aa87b1389
https://hdl.handle.net/11368/2721897
https://hdl.handle.net/11368/2721897
Mélanges originated from sedimentary processes (sedimentary mélanges) and olistostromes are frequently present in mountain chains worldwide. They are excellent fossil examples of mass-transport complexes (MTC), often cropping out in well-preserved
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::9dc09ec22cfbf6f6180c49719458d5f9
https://hdl.handle.net/11368/2695840
https://hdl.handle.net/11368/2695840
Autor:
PINI, GIAN ANDREA, Festa A., Ogata K., CAMERLENGHI, ANGELO, Cowan D. S., Dilek Y., Lucente C. C.
Due to the recent advances in the investigating methods and the increasing work of comparison between mélanges in mountain chains worldwide, several mèlanges are now recognized as mass-transport complexes (MTCs), variously deformed by post-depositi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::295dcda30b9d62a7217d4dad0f18609e
http://hdl.handle.net/2318/119850
http://hdl.handle.net/2318/119850
Autor:
Pini, G. A., Camerlenghi, A., Kei Ogata, Festa, A., Codegone, G., Lucente, C. C., Urgeles, R.
Publikováno v:
Scopus-Elsevier
CIÊNCIAVITAE
CIÊNCIAVITAE
The terms olistostrome and olistolith have been introduced by G. Flores (4th World Petroleum Congress, 1955, Rome) to indicate either sedimentary bodies with a chaotic block-in-Matrix fabric or single slide blocks, intercalated between layered sequen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::4c15dc6642a3d99dcf22a3e718909c28
https://hdl.handle.net/11368/2695819
https://hdl.handle.net/11368/2695819
Publikováno v:
Scopus-Elsevier
The Modino complex is a composite chaotic body, more than 400 m thick, extending for more than 50bkilometers. It is intercalated within the lower Miocene turbidite succession of the Northern Apennines. The sedimentary versus tectonic mechanism of emp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::02be1ee9f5d71f4054738e2495173fe1
https://hdl.handle.net/11368/2695833
https://hdl.handle.net/11368/2695833
Autor:
Lucente, C. C., Pini, GIAN ANDREA
Due to the good exposures and the already available, detailed stratigraphic and geological data, the Marnoso-arenacea Formation represents a unique opportunity for the study of the overall geometry and internal organization of slide bodies and relate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::70cb03d1962509dbdbd91bfdd7e55873
http://hdl.handle.net/11585/21771
http://hdl.handle.net/11585/21771