Zobrazeno 1 - 10
of 16
pro vyhledávání: '"Epiligurian succession"'
Publikováno v:
Submarine Mass Movements and Their Consequences-5th International Symposium, 595-605
STARTPAGE=595;ENDPAGE=605;TITLE=Submarine Mass Movements and Their Consequences-5th International Symposium
Ogata, K, Tinterri, R, Pini, G A & Mutti, E 2012, The specchio unit (northern apennines, Italy): An ancient mass transport complex originated from near-coastal areas in an intra-slope setting . in Submarine Mass Movements and Their Consequences-5th International Symposium . Submarine Mass Movements and Their Consequences-5th International Symposium, Kluwer Academic Publishers., pp. 595-605 . https://doi.org/10.1007/978-94-007-2162-3_53
Submarine Mass Movements and Their Consequences ISBN: 9789400721616
STARTPAGE=595;ENDPAGE=605;TITLE=Submarine Mass Movements and Their Consequences-5th International Symposium
Ogata, K, Tinterri, R, Pini, G A & Mutti, E 2012, The specchio unit (northern apennines, Italy): An ancient mass transport complex originated from near-coastal areas in an intra-slope setting . in Submarine Mass Movements and Their Consequences-5th International Symposium . Submarine Mass Movements and Their Consequences-5th International Symposium, Kluwer Academic Publishers., pp. 595-605 . https://doi.org/10.1007/978-94-007-2162-3_53
Submarine Mass Movements and Their Consequences ISBN: 9789400721616
Within the Eocene-Oligocene syn-orogenic deposits of the Epiligurian succession (Northern Apennines of Italy), a field-based study of the Specchio Unit (lower Rupelian) reveals that this complex is made up of three distinct but amalgamated mass- Tran
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::76a9761cf39fb273d3e14148e54d54e5
https://research.vu.nl/en/publications/16e03152-df3f-4a82-ba3b-fad693eba4fc
https://research.vu.nl/en/publications/16e03152-df3f-4a82-ba3b-fad693eba4fc
Within the Eocene-Oligocene syn-orogenic deposits of the Epiligurian succession (Northern Apennines of Italy), a field-based study of the Specchio Unit (lower Rupelian) reveals that this complex is made up by the amalgamation of 3 distinct mass-trans
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::0f5aca31fc4e1ee5d2330a267886e83f
http://hdl.handle.net/11368/2695841
http://hdl.handle.net/11368/2695841
Autor:
Ogata, Kei
Il recente incremento dell’esplorazione geofisica dei margini continentali e il concomitante sviluppo di tecnologie d’indagine, sismiche ed acustiche, sempre più accurate, hanno rivelato la comune presenza di vasti accumuli di sedimenti rimobili
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______341::6a72d38dfd0b228eb13bd5511aa9dc4a
http://hdl.handle.net/1889/1388
http://hdl.handle.net/1889/1388
Autor:
Pini, GIAN ANDREA
Rocks characterized by an apparently chaotic block in matrix fabric and known as argille scagliose are widespread in the Apennines of Italy. Most of the argille scagliose can be differentiated into two kinds of units, tectonosomes and olistostromes,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::c78aa988e879afe9ce18f1807356d005
https://hdl.handle.net/11368/2695974
https://hdl.handle.net/11368/2695974
A volcanoclastic ash-layer, 1 m thick, has been found interbedded in the Antognola Formation (Epiligurian successions, Oligo-Miocene) in the Sillaro riverbed (Bologna foothils, Northern Apennines). Five micropaleontological samples have provided a Ch
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::38c95265921cb7ba9902fbb34ab4ff62
https://hdl.handle.net/11368/2695848
https://hdl.handle.net/11368/2695848
Autor:
PINI, GIAN ANDREA
The Argille Scagliose complex of the Northern Apennines have been recently subdivided in tectonics and olistostromes, both characterized by a “block in clayey matrix” texture. Tectonite units derive from tectonic lamination of an lower Cretaceous
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::8da59e04f46bd33fbe0120e2ed35996c
http://hdl.handle.net/11368/2696026
http://hdl.handle.net/11368/2696026
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