(Table 1) Strontium isotopic ratios of interstitial waters from ODP Leg 125 holes

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Auteurs principaux: Haggerty, Janet A, Chaudhuri, Sambhudas
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 1992
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author Haggerty, Janet A
Chaudhuri, Sambhudas
author_facet Haggerty, Janet A
Chaudhuri, Sambhudas
collection Datos científicos de ciencias marinas y ambientales
contents The strontium isotopic data presented here are from interstitial waters squeezed from unconsolidated serpentine, an unusual type of substrate that was recovered from Mariana and Bonin forearc seamounts and has not been previously drilled by the Deep Sea Drilling Project or Ocean Drilling Program. The texture and composition of some of these serpentine deposits from Conical Seamount, located on the Mariana forearc, indicate emplacement as low- or high-viscosity, cold gravitational flows, which are therefore neither sediment nor igneous rock. The strontium isotopic ratios of the interstitial waters from the unconsolidated serpentine range from 0.70912 to 0.70525 and trend toward a relatively less radiogenic composition with increasing sub-bottom depth. These strontium isotopic ratios are derived from at least two strontium sources: seawater and igneous. The strontium isotopic gradients from the interstitial waters from the Leg 125 sites are probably the result of diffusive transport of strontium from an igneous source deep within the lithosphere that may be contaminated with subducted or underplated sediment.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_770845
institution PANGAEA
language en
publishDate 1992
publisher PANGAEA
record_format pangaea
spellingShingle (Table 1) Strontium isotopic ratios of interstitial waters from ODP Leg 125 holes
Haggerty, Janet A
Chaudhuri, Sambhudas
125-779A; 125-780C; 125-781A; 125-784A; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Isotope ratio mass spectrometry; Joides Resolution; Leg125; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label; Strontium-87/Strontium-86 ratio; Strontium-87/Strontium-86 ratio, error
The strontium isotopic data presented here are from interstitial waters squeezed from unconsolidated serpentine, an unusual type of substrate that was recovered from Mariana and Bonin forearc seamounts and has not been previously drilled by the Deep Sea Drilling Project or Ocean Drilling Program. The texture and composition of some of these serpentine deposits from Conical Seamount, located on the Mariana forearc, indicate emplacement as low- or high-viscosity, cold gravitational flows, which are therefore neither sediment nor igneous rock. The strontium isotopic ratios of the interstitial waters from the unconsolidated serpentine range from 0.70912 to 0.70525 and trend toward a relatively less radiogenic composition with increasing sub-bottom depth. These strontium isotopic ratios are derived from at least two strontium sources: seawater and igneous. The strontium isotopic gradients from the interstitial waters from the Leg 125 sites are probably the result of diffusive transport of strontium from an igneous source deep within the lithosphere that may be contaminated with subducted or underplated sediment.
title (Table 1) Strontium isotopic ratios of interstitial waters from ODP Leg 125 holes
topic 125-779A; 125-780C; 125-781A; 125-784A; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Isotope ratio mass spectrometry; Joides Resolution; Leg125; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label; Strontium-87/Strontium-86 ratio; Strontium-87/Strontium-86 ratio, error
url https://doi.org/10.1594/PANGAEA.770845