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Autor:
Boschi C. [1], Bonatti E. [2, Ligi M. [2], Brunelli D. [2, Cipriani A. [3, 4] Dallai L. [1], D'Orazio M. [5], Früh-Green L. [6], Tonarini S. [1], Barnes J. [7], Bedini R. [8]
Publikováno v:
Lithos (Oslo. Print) 178 (2013): 3–23. doi:10.1016/j.lithos.2013.06.003
info:cnr-pdr/source/autori:Boschi C. [1], Bonatti E. [2, 3], Ligi M. [2], Brunelli D. [2, 3], Cipriani A. [3, 4] Dallai L. [1], D'Orazio M. [5], Früh-Green L. [6], Tonarini S. [1], Barnes J. [7], Bedini R. [8]/titolo:Serpentinization of mantle peridotites along an uplifted lithospheric section, Mid Atlantic Ridge at 11° N./doi:10.1016%2Fj.lithos.2013.06.003/rivista:Lithos (Oslo. Print)/anno:2013/pagina_da:3/pagina_a:23/intervallo_pagine:3–23/volume:178
LITHOS
info:cnr-pdr/source/autori:Boschi C. [1], Bonatti E. [2, 3], Ligi M. [2], Brunelli D. [2, 3], Cipriani A. [3, 4] Dallai L. [1], D'Orazio M. [5], Früh-Green L. [6], Tonarini S. [1], Barnes J. [7], Bedini R. [8]/titolo:Serpentinization of mantle peridotites along an uplifted lithospheric section, Mid Atlantic Ridge at 11° N./doi:10.1016%2Fj.lithos.2013.06.003/rivista:Lithos (Oslo. Print)/anno:2013/pagina_da:3/pagina_a:23/intervallo_pagine:3–23/volume:178
LITHOS
Mantle peridotites from an exposed lithospheric section (Vema Lithospheric Section, VLS), generated during ~ 26 Ma at a ~ 80 km long Mid Atlantic Ridge segment (11° N), have been sampled and studied to understand the evolution of the serpentinizatio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::09afaf53d33b0efb52c186ab96c4dd24
https://hdl.handle.net/11380/969910
https://hdl.handle.net/11380/969910