10.1594/PANGAEA.711026
Benton, Laurie D
Laurie D
Benton
Ryan, Jeffrey
Jeffrey
Ryan
0000-0003-3969-1761
Tera, Fouad
Fouad
Tera
Boron isotope ratios of samples from ODP Leg 125 sites at a serpentine seamount, Mariana forearc
PANGAEA
2001
Drilling/drill rig
Leg125
Joides Resolution
Ocean Drilling Program (ODP)
1989-02-27T23:30:00/1989-03-10T23:45:00
en
Supplementary Publication Series of Datasets
10.1016/S0012-821X(01)00286-2
2 datasets
application/zip
Creative Commons Attribution 3.0 Unported
Serpentinite clasts and muds erupted from Conical Seamount, Mariana forearc, show substantial enrichment in boron (B) and 11B (delta11B up to +15 per mil ) relative to mantle values. These elevated B isotope signatures result from chemical exchange with B-rich pore fluids that are upwelling through the seamount. If the trends of decreasing delta11B with slab depth shown by cross-arc magmatic suites in the Izu and Kurile arcs of the western Pacific are extended to shallow depths (~25 km), they intersect the inferred delta11B of the slab-derived fluids (+13x) at Conical Seamount. Simple mixtures of a B-rich fluid with a high delta11B and B-poor mantle with a low delta11B are insufficient to explain the combined forearc and arc data sets. The B isotope systematics of subduction-related rocks thus indicate that the fluids evolved from downgoing slabs are more enriched in 11B than the slab materials from which they originate. Progressively lower delta11B in arc lavas erupted above deep slabs reflects both the progressive depletion of 11B from the slab and progressively greater inputs of mantle-derived B. This suggests that the slab releases 11B-enriched fluids from the shallowest levels to depths greater than 200 km.
Supplement to: Benton, Laurie D; Ryan, Jeffrey; Tera, Fouad (2001): Boron isotope systematics of slab fluids as inferred from a serpentine seamount, Mariana forearc. Earth and Planetary Science Letters, 187(3-4), 273-282
146.6533
146.696
19.5125
19.5425
North Pacific Ocean