Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Mass transport processe"'
Autor:
Kei Ogata, Angelo Camerlenghi, Giulia Codegone, Gian Andrea Pini, Andrea Festa, Claudio Corrado Lucente
Publikováno v:
Sedimentary melanges and fossil mass-Transport complexes: A key for better understanding submarine mass movements?, 31, 585-594
Submarine Mass Movements and Their Consequences ISBN: 9789400721616
Pini, G A, Ogata, K, Camerlenghi, A, Festa, A, Lucente, C C & Codegone, G 2012, Sedimentary Melanges and Fossil Mass-Transport Complexes: A Key for Better Understanding Submarine Mass Movements? in Sedimentary melanges and fossil mass-Transport complexes: A key for better understanding submarine mass movements? . vol. 31, Submarine Mass Movements and Their Consequences-5th International Symposium, Springer International Publishing Switzerland, pp. 585-594 . https://doi.org/10.1007/978-94-007-2162-3_52
Submarine Mass Movements and Their Consequences ISBN: 9789400721616
Pini, G A, Ogata, K, Camerlenghi, A, Festa, A, Lucente, C C & Codegone, G 2012, Sedimentary Melanges and Fossil Mass-Transport Complexes: A Key for Better Understanding Submarine Mass Movements? in Sedimentary melanges and fossil mass-Transport complexes: A key for better understanding submarine mass movements? . vol. 31, Submarine Mass Movements and Their Consequences-5th International Symposium, Springer International Publishing Switzerland, pp. 585-594 . https://doi.org/10.1007/978-94-007-2162-3_52
Although the 1978 Penrose Conference stated that “Mélanges are mappable, internally fragmented and mixed rock bodies” formed by “tectonic movements, sedimentary sliding, or any combination of such processes”, an exclusive origin from tectoni
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::55d47945c3df455bb1fc3e70c4d9a642
https://research.vu.nl/en/publications/8004a86e-fd66-4d67-bac9-7deb12aeba12
https://research.vu.nl/en/publications/8004a86e-fd66-4d67-bac9-7deb12aeba12
Publikováno v:
Tectonophysics, 568-569, 185-199. Elsevier
Ogata, K, Mutti, E, Pini, G A & Tinterri, R 2012, ' Mass transport-related stratal disruption within sedimentary m??langes: Examples from the northern Apennines (Italy) and south-central Pyrenees (Spain) ', Tectonophysics, vol. 568-569, pp. 185-199 . https://doi.org/10.1016/j.tecto.2011.08.021
Ogata, K, Mutti, E, Pini, G A & Tinterri, R 2012, ' Mass transport-related stratal disruption within sedimentary m??langes: Examples from the northern Apennines (Italy) and south-central Pyrenees (Spain) ', Tectonophysics, vol. 568-569, pp. 185-199 . https://doi.org/10.1016/j.tecto.2011.08.021
We report here mass transport-related disruption processes and their artifacts within sedimentary m??langes. The case studies include the early Oligocene wedge-top mass transport deposits in the northern Apennines (Italy) and the Eocene foredeep carb
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d8412c098b39fc35a6b58f79fc1d87dd
https://research.vu.nl/en/publications/85f3098c-9032-4b72-9974-b1bea465bd47
https://research.vu.nl/en/publications/85f3098c-9032-4b72-9974-b1bea465bd47
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
Mass-transport deposits, olistostromes and mélanges represent significant components of both modern and ancient continental margins. Tectonic forces and processes constitute the most common triggering mechanisms to downslope movement and formation o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::b6b19a7ad727124a75d0a0eca5916dac
http://hdl.handle.net/11585/126886
http://hdl.handle.net/11585/126886
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