Straub, Susanne M; Layne, Graham D (2003): Geochemistry of fallout tephra from ODP Hole 125-782A. PANGAEA, https://doi.org/10.1594/PANGAEA.780330, Supplement to: Straub, SM; Layne, GD (2003): Decoupling of fluids and fluid-mobile elements during shallow subduction: Evidence from halogen-rich andesite melt inclusions from the Izu arc volcanic front. Geochemistry, Geophysics, Geosystems, 4(7), 9003, https://doi.org/10.1029/2002GC000349
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Very rare, halogen-rich andesite melt inclusions (HRA) in bytownitic plagioclase phenocrysts (An89–90) from tephra fallout of the Izu arc volcanic front (Izu VF) provide new insights into the processes of fluid release from slab trenchward to the volcanic front in a cool subduction zone. These HRA are markedly enriched in Cl, F and Li - by factors of up to 8 (Cl, F) and 1.5 (Li) - but indistinguishable with respect to the fluid-mobile large-ion lithophile elements (LILE; K, Sr, Rb, Cs, Ba, Pb, U), rare earths (REE) or high field strength elements (HFSE) from the low-K tholeiitic magmas of the Izu VF. We suggest that the chemical signature of the HRA reflects the presence of a fluid in the mantle source that originated from the serpentinized mantle peridotite above the metacrust. This “wedge serpentinite” presumably formed by fluid infiltration beneath the forearc and was subsequently down-dragged with the slab to arc front depths. The combined evidence from the Izu VF (?110 km above slab) and the outer forearc serpentinite seamounts (~25 to 30 km above slab) suggests that the slab flux of B and Cl is highest beneath the forearc, and decreases with increasing slab depths. In contrast, the slab flux of Li is minor beneath the forearc, but increases with depth. Fluorine may behave similarly to Li, whereas the fluid-mobile LILE appear to be largely retained in the slab trenchward from the Izu VF. Consequently, the chemical signatures of both Izu trench sediments and basaltic rocks appear preserved until arc front depths.
Latitude: 30.861000 * Longitude: 141.314200
Date/Time Start: 1989-03-16T18:00:00 * Date/Time End: 1989-03-17T07:30:00
125-782A * Latitude: 30.861000 * Longitude: 141.314200 * Date/Time Start: 1989-03-16T18:00:00 * Date/Time End: 1989-03-17T07:30:00 * Elevation: -2958.9 m * Penetration: 476.8 m * Recovery: 282 m * Location: North Pacific Ocean * Campaign: Leg125 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 50 cores; 476.8 m cored; 0 m drilled; 59.1 % recovery
Datasets listed in this publication series
- Straub, SM; Layne, GD (2003): (Table 1) Composition of matrix glasses from ODP 125-782A fallout tephra. https://doi.org/10.1594/PANGAEA.780321
- Straub, SM; Layne, GD (2003): (Table 2) Composition of matrix shards and melt inclusions in fallout tephra from ODP 125-782A. https://doi.org/10.1594/PANGAEA.780327
- Straub, SM; Layne, GD (2003): (Table 3) Composition of halogen-rich andesites and normal group glasses from ODP 125-782A fallout tephra. https://doi.org/10.1594/PANGAEA.780328
- Straub, SM; Layne, GD (2003): (Table 4) Composition of halogen-rich andesites and mixed rhyolite inclusion fallout tephra from ODP 125-782A. https://doi.org/10.1594/PANGAEA.780329