Zobrazeno 1 - 10
of 23
pro vyhledávání: '"Luca C. Malatesta"'
In 1978, Ōta and Yoshikawa published a pioneering study describing four distinct zones of marine terrace patterns in Japan and linked them to the large geodynamic processes controlling deformation across the arc. We repeat the exercise of Ōta and Y
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::97fa7f1066a64d7d11dbdf51976878cf
https://doi.org/10.5194/egusphere-egu23-10899
https://doi.org/10.5194/egusphere-egu23-10899
Publikováno v:
Proceedings of the National Academy of Sciences, vol. 119, no. 13
Proceedings of the National Academy of Sciences of the United States of America (PNAS)
Proceedings of the National Academy of Sciences of the United States of America (PNAS)
Erosion and sedimentation constantly rework topography created by tectonics but also modulate stresses in the underlying crust by redistributing surficial loads. Decades of numerical modeling further suggest that surface processes help focus deformat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::571f13969ef0b5995848a4a2359f3640
https://serval.unil.ch/notice/serval:BIB_0984228D4065
https://serval.unil.ch/notice/serval:BIB_0984228D4065
Autor:
Luca C. Malatesta, Kimberly L. Huppert
Crustal deformation along active coastline can be constrained with age and elevation of marine terraces. These are essentially the product of an erosive process (waves eroding bedrock) and a preservation process (rock uplift moving terraces up and aw
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::587249b82b652fa2e2b77e110c3e7b99
https://doi.org/10.5194/egusphere-egu22-11284
https://doi.org/10.5194/egusphere-egu22-11284
Publikováno v:
Geology
Geology, vol. 50, no. 1, pp. 101-105
Geology, vol. 50, no. 1, pp. 101-105
Marine terraces are a cornerstone for the study of paleo sea level and crustal deformation. Commonly, individual erosive marine terraces are attributed to unique sea-level high stands based on the reasoning that marine platforms could only be signifi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::65dd0dcc6ad2f71fb89e8d0056feed9e
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5008429_2/component/file_5009717/5008429.pdf
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5008429_2/component/file_5009717/5008429.pdf
Autor:
Alex Hughes, Javier Escartín, Frédérique Leclerc, Christine Deplus, Luca C. Malatesta, Jean-Arthur Olive, Jérémy Billant, N. Feuillet
Publikováno v:
Journal Of Geophysical Research-earth Surface (2169-9003) (American Geophysical Union (AGU)), 2021-04, Vol. 126, N. 4, P. e2020JF005892 (25p.)
Journal of Geophysical Research: Earth Surface
Journal of Geophysical Research: Earth Surface, 2021, 126 (4), ⟨10.1029/2020JF005892⟩
Journal of Geophysical Research: Earth Surface, American Geophysical Union/Wiley, 2021, 126 (4), ⟨10.1029/2020JF005892⟩
Journal of Geophysical Research: Earth Surface
Journal of Geophysical Research: Earth Surface, 2021, 126 (4), ⟨10.1029/2020JF005892⟩
Journal of Geophysical Research: Earth Surface, American Geophysical Union/Wiley, 2021, 126 (4), ⟨10.1029/2020JF005892⟩
Due to challenges involved in mapping the seafloor at high‐resolution (e.g., < 2 m), data are lacking to understand processes that control the evolution of submarine normal fault scarps, which cover large parts of the global seafloor. Here, we use
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::db4d48ff0d698931c293ce5b0cfa7a6a
https://archimer.ifremer.fr/doc/00684/79578/
https://archimer.ifremer.fr/doc/00684/79578/
Sequences of coral reef terraces result from the interplay between biogenic and clastic sedimentary production, relative sea level (RSL) variations, wave erosion and tectonic forcing. Reefal sequences are gold standard proxies for paleo-sea level and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6cbe725d2900ef14bfe37fa94afb8c70
https://doi.org/10.5194/egusphere-egu21-15976
https://doi.org/10.5194/egusphere-egu21-15976
Marine terraces are a cornerstone for the study of paleo sea level and crustal deformation. Commonly, individual erosive marine terraces are attributed to unique sea level high-stands. This stems from early reasoning that marine platforms could only
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2ad5ea475fa84e2c4c8069cbb8c780d2
https://doi.org/10.5194/egusphere-egu21-9076
https://doi.org/10.5194/egusphere-egu21-9076
Models that couple tectonics and surface processes commonly predict that efficient erosion and sedimentation help focus crustal deformation onto fewer, longer-lived faults. However, because their geomorphic parameters are difficult to calibrate again
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ee8a7f6ab08c2080c8f7035c1ab50339
https://doi.org/10.5194/egusphere-egu21-5193
https://doi.org/10.5194/egusphere-egu21-5193
Publikováno v:
Journal of Geophysical Research : Solid Earth
Journal of Geophysical Research : Solid Earth, American Geophysical Union, 2021, 126 (1), pp.e2020JB019589. ⟨10.1029/2020JB019589⟩
Journal of Geophysical Research: Solid Earth
Journal of Geophysical Research: Solid Earth, vol. 126, no. 1
Journal of Geophysical Research : Solid Earth, American Geophysical Union, 2021, 126 (1), pp.e2020JB019589. ⟨10.1029/2020JB019589⟩
Journal of Geophysical Research: Solid Earth
Journal of Geophysical Research: Solid Earth, vol. 126, no. 1
International audience; Along subduction margins, the morphology of the near shore domain records the combined action of erosion from ocean waves and permanent tectonic deformation from the convergence of plates. We observe that at subduction margins
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::41026afa820067f3cf2330de97b6ef39
https://hal.archives-ouvertes.fr/hal-03342203/file/2020JB019589.pdf
https://hal.archives-ouvertes.fr/hal-03342203/file/2020JB019589.pdf
Autor:
Léo Petit, Roger Buck, Luca C. Malatesta, Jean-Arthur Olive, Julie Oppenheimer, Lucile Bruhat, Antoine Demont, P. M. Betka
Tectonic plate boundaries are shaped by localized and distributed brittle-plastic deformation such as slip on major faults and folding of fault-bounded blocks. However, the microstructural to outcrop-scale mechanisms that enable such deformation and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::268da386a9035621043e4b21927ca121
https://doi.org/10.5194/egusphere-egu2020-5020
https://doi.org/10.5194/egusphere-egu2020-5020