Chemistry of interstitial water of samples from DSDP Leg 38

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Auteurs principaux: Gieskes, Joris M, Lawrence, James R, Galleisky, Guntwin
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 1976
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author Gieskes, Joris M
Lawrence, James R
Galleisky, Guntwin
author_facet Gieskes, Joris M
Lawrence, James R
Galleisky, Guntwin
collection Datos científicos de ciencias marinas y ambientales
contents Interstitial waters recovered during Leg 38 show large changes in major ion composition and also in oxygen isotope composition. Increases in Ca[++] and Sr[++] and decreases in K[+], Mg[++], and O18/O16 are interpreted in terms of extensive diagenesis of terrigenous, volcanic, or basaltic igneous materials in the sediments and underlying basalts. Slight, but well-established increases in chlorinity with depth indicate that these postulated weathering reactions involve uptake of water to a measurable extent. Interstitial waters from sites drilled on the Inner Voring Plateau suggest the infusion of fresh waters by aquifers from the mainland of Norway.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_710841
institution PANGAEA
language en
publishDate 1976
publisher PANGAEA
record_format pangaea
spellingShingle Chemistry of interstitial water of samples from DSDP Leg 38
Gieskes, Joris M
Lawrence, James R
Galleisky, Guntwin
38-336; 38-337; 38-338; 38-339; 38-340; 38-341; 38-342; 38-343; 38-344; 38-345; 38-346; 38-348; 38-349; 38-350; 38-352_Site; COMPCORE; Composite Core; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg38; North Atlantic/Greenland Sea/RIDGE; North Atlantic/Norwegian Sea; North Atlantic/Norwegian Sea/BASIN; North Atlantic/Norwegian Sea/DIAPIR; North Atlantic/Norwegian Sea/PLATEAU; North Atlantic/Norwegian Sea/RIDGE; North Atlantic/RIDGE
Interstitial waters recovered during Leg 38 show large changes in major ion composition and also in oxygen isotope composition. Increases in Ca[++] and Sr[++] and decreases in K[+], Mg[++], and O18/O16 are interpreted in terms of extensive diagenesis of terrigenous, volcanic, or basaltic igneous materials in the sediments and underlying basalts. Slight, but well-established increases in chlorinity with depth indicate that these postulated weathering reactions involve uptake of water to a measurable extent. Interstitial waters from sites drilled on the Inner Voring Plateau suggest the infusion of fresh waters by aquifers from the mainland of Norway.
title Chemistry of interstitial water of samples from DSDP Leg 38
topic 38-336; 38-337; 38-338; 38-339; 38-340; 38-341; 38-342; 38-343; 38-344; 38-345; 38-346; 38-348; 38-349; 38-350; 38-352_Site; COMPCORE; Composite Core; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg38; North Atlantic/Greenland Sea/RIDGE; North Atlantic/Norwegian Sea; North Atlantic/Norwegian Sea/BASIN; North Atlantic/Norwegian Sea/DIAPIR; North Atlantic/Norwegian Sea/PLATEAU; North Atlantic/Norwegian Sea/RIDGE; North Atlantic/RIDGE
url https://doi.org/10.1594/PANGAEA.710841