Zobrazeno 1 - 2
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pro vyhledávání: '"Sanfilippo A.[2"'
Publikováno v:
Journal of Geophysical Research : Solid Earth
Journal of Geophysical Research : Solid Earth, American Geophysical Union, 2021, 126 (9), pp.e2021JB022215. ⟨10.1029/2021jb022215⟩
Journal of geophysical research. Solid earth
126 (2021): 1–23. doi:10.1029/2021JB022215
info:cnr-pdr/source/autori:Casini L.[1], Maino M.[2,3], Sanfilippo A.[2,3], Ildefonse B.[4], Dick H.J.B.[5]/titolo:High-Temperature Strain Localization and the Nucleation of Oceanic Core Complexes (16.5°N, Mid-Atlantic Ridge)/doi:10.1029%2F2021JB022215/rivista:Journal of geophysical research. Solid earth (Print)/anno:2021/pagina_da:1/pagina_a:23/intervallo_pagine:1–23/volume:126
Journal of Geophysical Research : Solid Earth, American Geophysical Union, 2021, 126 (9), pp.e2021JB022215. ⟨10.1029/2021jb022215⟩
Journal of geophysical research. Solid earth
126 (2021): 1–23. doi:10.1029/2021JB022215
info:cnr-pdr/source/autori:Casini L.[1], Maino M.[2,3], Sanfilippo A.[2,3], Ildefonse B.[4], Dick H.J.B.[5]/titolo:High-Temperature Strain Localization and the Nucleation of Oceanic Core Complexes (16.5°N, Mid-Atlantic Ridge)/doi:10.1029%2F2021JB022215/rivista:Journal of geophysical research. Solid earth (Print)/anno:2021/pagina_da:1/pagina_a:23/intervallo_pagine:1–23/volume:126
International audience; Extension at slow to ultraslow midoceanic ridges is mostly accommodated by large detachment faults that expose mantle peridotite and/or lower-crustal rocks forming Oceanic Core Complexes (OCC). It is commonly accepted that OCC
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7254c86c4a1ad526d26dea6730326e4f
https://doi.org/10.1029/2021jb022215
https://doi.org/10.1029/2021jb022215
Autor:
Rampone E.[1], Sanfilippo A.[2
Publikováno v:
Elements (Que. Online) 17 (2021): 23–28. doi:10.2138/GSELEMENTS.17.1.23
info:cnr-pdr/source/autori:Rampone E.[1], Sanfilippo A.[2,3]/titolo:The heterogeneous tethyan oceanic lithosphere of the alpine ophiolites/doi:10.2138%2FGSELEMENTS.17.1.23/rivista:Elements (Que. Online)/anno:2021/pagina_da:23/pagina_a:28/intervallo_pagine:23–28/volume:17
info:cnr-pdr/source/autori:Rampone E.[1], Sanfilippo A.[2,3]/titolo:The heterogeneous tethyan oceanic lithosphere of the alpine ophiolites/doi:10.2138%2FGSELEMENTS.17.1.23/rivista:Elements (Que. Online)/anno:2021/pagina_da:23/pagina_a:28/intervallo_pagine:23–28/volume:17
The Alpine–Apennine ophiolites are lithospheric remnants of the Jurassic Alpine Tethys Ocean. They predominantly consist of exhumed mantle peridotites with lesser gabbroic and basaltic crust and are locally associated with continental crustal mater
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::29d23da8afab0fd69126e29d24e904fc
http://hdl.handle.net/11567/1050057
http://hdl.handle.net/11567/1050057
