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Behavior of Li and its isotopes during serpentinization of oceanic peridotites ArchiMer
Decitre, S; Deloule, E; Reisberg, L; James, R; Agrinier, P; Mevel, C.
[1] Analyses of Li and Li isotopes in serpentinized peridotites have been performed using Thermo-Ionisation Mass Spectrometry (TIMS) and Secondary Ion Mass Spectrometry (SIMS) techniques on samples collected from the southwest Indian Ridge (SWIR). In the bulk samples, Li concentrations range from 0.6 to 8.2 ppm, while whole rock delta(6)Li values range from -2.9 to -14parts per thousand. In situ analyses display a greater range in both Li concentration (0.1-19.5 ppm) and Li isotopic composition ( -27 to +19parts per thousand), with the serpentinized portions having higher Li concentrations than the associated relict phases. These variations may reflect changes in Li partitioning and isotopic fractionation between serpentine and fluid with temperature and...
Tipo: Text Palavras-chave: Lithium; Isotopes; Geochemical cycle; Oceanic crust; Serpentinization.
Ano: 2002 URL: https://archimer.ifremer.fr/doc/00223/33403/31860.pdf
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Evidence for major-element heterogeneity in the mantle source of abyssal peridotites from the Southwest Indian Ridge (52 degrees to 68 degrees E) ArchiMer
Seyler, M; Cannat, M; Mevel, C.
A suite of 53 samples of mantle spinel lherzolites and harzburgites dredged at 13 sites between 52degreesE and 68degreesE along the Southwest Indian Ridge has been studied for petrography and mineral major element chemistry. Results show that the residual mantle beneath this very slow-spreading/cold ridge is strongly heterogeneous in modal and mineral compositions at local and regional scales and underwent greater extents of melting than predicted by melting model and by compositions of the basalts dredged with the peridotites. Along-axis, the peridotite compositional variability defines a concave pattern with increasing depletion at both ends of the studied section (e. g., approaching Rodrigues Triple Junction to the East and Gallieni fracture zone to the...
Tipo: Text Palavras-chave: Peridotite midocean ridge Indian Ocean petrology mantle heterogeneity geochemistry : composition of the mantle marine geology and geophysics : midocean ridge processes information related to geographic region : Indian Ocean history of geophysics : volcanology; Geochemistry; And petrology.
Ano: 2003 URL: https://archimer.ifremer.fr/doc/00224/33506/31941.pdf
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FUJI Dome: A large detachment fault near 64 degrees E on the very slow-spreading southwest Indian Ridge ArchiMer
Searle, Rc; Cannat, M; Fujioka, K; Mevel, C; Fujimoto, H; Bralee, A; Parson, L.
A continuous, domed detachment surface ( FUJI Dome) has been imaged on the very slow-spreading southwest Indian Ridge using deep-towed side-scan sonar, and has been investigated by manned submersible and sea-surface geophysics. The Dome is morphologically similar to other oceanic detachments, core complexes or mega-mullions. In addition to bathymetric mullions observed in ship-borne bathymetry, finer scale spreading-parallel striations were imaged with the side scan. On the detachment surface, metabasalt crops out near the termination, probably as part of a thin fault sliver. Gabbro and troctolite probably crop out near the summit of the dome. The rest of the detachment surface is covered with sediment and rubble which is basaltic except for a single...
Tipo: Text Palavras-chave: Southwest Indian Ridge; Detachment; Submersible; Magnetic; Gravity; Marine geology and geophysics : midocean ridge processes; Marine geology and geophysics :; Seafloor morphology and bottom photography.
Ano: 2003 URL: https://archimer.ifremer.fr/doc/00226/33706/32124.pdf
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New insights into the origin and distribution of the DUPAL isotope anomaly in the Indian Ocean mantle from MORB of the Southwest Indian Ridge ArchiMer
Meyzen, Cm; Ludden, Jn; Humler, E; Luais, B; Toplis, Mj; Mevel, C; Storey, M.
We report new Sr, Nd, and Pb isotope data for Mid-Ocean Ridge Basalts (MORB) dredged between 35 and 69 degrees E along a similar to 4100 km section of the Southwest Indian Ridge (SWIR), which is one of the slowest spreading ridges of the global mid-ocean ridge system ( full rate of 16 mm yr(-1)). The SWIR appears isotopically more heterogeneous than other mid-ocean ridges over similar length scales and comparable sampling density. Isotopic variations are generally independent of ridge segmentation, and the degree of heterogeneity decreases from west to east. This decrease in heterogeneity correlates with the observed increase in axial depth and decrease in crustal thickness, commonly attributed to decreasing mantle potential temperature. Data for the...
Tipo: Text Palavras-chave: Southwest Indian Ridge; MORB; Isotopes; Indian Ocean; Lower crust; Mantle.
Ano: 2005 URL: https://archimer.ifremer.fr/doc/00232/34286/32655.pdf
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