Výsledky vyhledávání - "Brunelli D.[3"

Short-scale variability of the SCLM beneath the extra-Andean back-arc (Paso de Indios, Argentina): Evidence from spinel-facies mantle xenoliths

Autor: Ponce A.D.[1], Bertotto G.W.[1], Zanetti A.[2], Brunelli D.[3, Giovanardi T.[3, Aragon E. [6], Bernardi M.I.[1], Hemond C.[7] Mazzucchelli M.[2

Publikováno v: Open Geosciences 7 (2015): 362–385. doi:10.1515/geo-2015-0023
info:cnr-pdr/source/autori:Ponce A.D.[1], Bertotto G.W.[1], Zanetti A.[2], Brunelli D.[3,4], Giovanardi T.[3,5], Aragon E. [6], Bernardi M.I.[1], Hemond C.[7] Mazzucchelli M.[2,3]/titolo:Short-scale variability of the SCLM beneath the extra-Andean back-arc (Paso de Indios, Argentina): Evidence from spinel-facies mantle xenoliths/doi:10.1515%2Fgeo-2015-0023/rivista:Open Geosciences/anno:2015/pagina_da:362/pagina_a:385/intervallo_pagine:362–385/volume:7
Open Geosciences, Vol 7, Iss 1 (2015)
Open Geosciences (2391-5447) (Sciendo), 2015-01, Vol. 7, N. 1, P. 362-385
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
SEDICI (UNLP)
Universidad Nacional de La Plata
instacron:UNLP

Cenozoic basalts carrying ultramafic mantle xenoliths occur in the Matilde, León and Chenque hills in the Paso de Indios region, Argentina. The mantle xenoliths from the Chenque and León hills mainly present porphyroclastic textures, whereas the Ma

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::85e3369b82f0dbb41880ebee921aceb8
http://www.cnr.it/prodotto/i/345642

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26 Million Years of Mantle Upwelling Below a Segment of the Mid Atlantic Ridge: the Vema Lithospheric Section Revisited

Autor: Cipriani A (1), Bonatti E (1, 2, Brunelli D (3, Ligi M (4)

Publikováno v: Earth and planetary science letters 285 (2009): 87–95. doi:10.1016/j.epsl.2009.05.046
info:cnr-pdr/source/autori:Cipriani A (1), Bonatti E (1,2,4), Brunelli D (3,4), Ligi M (4)/titolo:26 million years of mantle upwelling below a segment of the Mid Atlantic Ridge: The Vema Lithospheric Section revisited/doi:10.1016%2Fj.epsl.2009.05.046/rivista:Earth and planetary science letters/anno:2009/pagina_da:87/pagina_a:95/intervallo_pagine:87–95/volume:285
Università degli studi di Modena e Reggio Emilia-IRIS

Temporal variations of temperature and composition of the mantle upwelling below a 80-km long segment of the Mid Atlantic Ridge were reconstructed from 20 to 4 Ma ago from peridotites sampled along a >300-km long section of oceanic lithosphere (Vema

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b0a714cadbacfbe00159964bfa4e2032
https://hdl.handle.net/11380/624558

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Stacked gabbro units and intervening mantle: A detailed look at a section of IODP Leg 305, Hole U1309D

Autor: Suhr G. (1), Hellebrand E. (2), Johnson K. (2), Brunelli D. (3

Publikováno v: 9 (2008): Q10007.
info:cnr-pdr/source/autori:Suhr G. (1), Hellebrand E. (2), Johnson K. (2), Brunelli D. (3,4)/titolo:Stacked gabbro units and intervening mantle: A detailed look at a section of IODP Leg 305, Hole U1309D/doi:/rivista:/anno:2008/pagina_da:Q10007/pagina_a:/intervallo_pagine:Q10007/volume:9

Hole U1309D (Integrated Ocean Drilling Program (IODP) Legs 304/305) penetrated 1415 m into the seafloor of the Atlantis Massif, an oceanic core complex at 30°N, Mid-Atlantic Ridge. More than 96% of all recovered rocks are gabbroic. On the basis of a

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::24dcbc9615f0df6eca8b94c39baf10f3
http://www.cnr.it/prodotto/i/49567

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