(Table 2) 87Sr/86Sr ratios of DSDP Site 38-336 samples ...

Interstitial waters of several sites drilled during the Deep Sea Drilling Project in the Norwegian-Greenland Sea during Leg 38 have revealed substantial changes in dissolved constituents and in the 18O/16O composition of interstitial waters. Studies of the chemical composition of the bulk sediments...

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Main Authors: Gieskes, Joris M, Lawrence, James R, Perry, Jr, Edward A, Grady, S J, Elderfield, Henry
Format: Dataset
Language:English
Published: PANGAEA 1987
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.705147
https://doi.pangaea.de/10.1594/PANGAEA.705147
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author Gieskes, Joris M
Lawrence, James R
Perry, Jr, Edward A
Grady, S J
Elderfield, Henry
author_facet Gieskes, Joris M
Lawrence, James R
Perry, Jr, Edward A
Grady, S J
Elderfield, Henry
author_sort Gieskes, Joris M
collection DataCite
description Interstitial waters of several sites drilled during the Deep Sea Drilling Project in the Norwegian-Greenland Sea during Leg 38 have revealed substantial changes in dissolved constituents and in the 18O/16O composition of interstitial waters. Studies of the chemical composition of the bulk sediments and their <1µm fraction indicate the presence of large amounts of volcanic ash, especially in sites close to Iceland. The presence of authigenic clay minerals (illite/smectite) suggests that alteration of this volcanic ash is an important process. A study of Site 348 reveals that dissolved Ca gradients are caused mainly by transport from the underlying basalts, but that decreases in Mg and d18O (H2O) are largely due to reactions involving alteration of volcanic ash in the sediments. Studies of 87Sr/86Sr distributions of dissolved Sr confirm this process in those sites with high contents of volcanic matter. On the other hand, in sites where the chemical composition of dissolved constituents has been little ... : Supplement to: Gieskes, Joris M; Lawrence, James R; Perry, Jr, Edward A; Grady, S J; Elderfield, Henry (1987): Chemistry of interstitial waters and sediments in the Norwegian-Greenland Sea, Deep Sea Drilling Project Leg 38. Chemical Geology, 63(1-2), 143-155 ...
format Dataset
genre Greenland
Greenland Sea
Iceland
genre_facet Greenland
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geographic Greenland
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institution Open Polar
language English
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op_doi https://doi.org/10.1594/pangaea.70514710.1016/0009-2541(87)90081-7
op_relation https://dx.doi.org/10.1016/0009-2541(87)90081-7
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
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publishDate 1987
publisher PANGAEA
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spelling ftdatacite:10.1594/pangaea.705147 2025-01-16T22:10:51+00:00 (Table 2) 87Sr/86Sr ratios of DSDP Site 38-336 samples ... Gieskes, Joris M Lawrence, James R Perry, Jr, Edward A Grady, S J Elderfield, Henry 1987 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.705147 https://doi.pangaea.de/10.1594/PANGAEA.705147 en eng PANGAEA https://dx.doi.org/10.1016/0009-2541(87)90081-7 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 DEPTH, sediment/rock Sample code/label Sample type Strontium-87/Strontium-86 ratio Strontium-87/Strontium-86 ratio, error Drilling/drill rig DSDP/ODP/IODP sample designation Leg38 Glomar Challenger Deep Sea Drilling Project DSDP dataset Supplementary Dataset Dataset 1987 ftdatacite https://doi.org/10.1594/pangaea.70514710.1016/0009-2541(87)90081-7 2024-08-01T10:58:30Z Interstitial waters of several sites drilled during the Deep Sea Drilling Project in the Norwegian-Greenland Sea during Leg 38 have revealed substantial changes in dissolved constituents and in the 18O/16O composition of interstitial waters. Studies of the chemical composition of the bulk sediments and their <1µm fraction indicate the presence of large amounts of volcanic ash, especially in sites close to Iceland. The presence of authigenic clay minerals (illite/smectite) suggests that alteration of this volcanic ash is an important process. A study of Site 348 reveals that dissolved Ca gradients are caused mainly by transport from the underlying basalts, but that decreases in Mg and d18O (H2O) are largely due to reactions involving alteration of volcanic ash in the sediments. Studies of 87Sr/86Sr distributions of dissolved Sr confirm this process in those sites with high contents of volcanic matter. On the other hand, in sites where the chemical composition of dissolved constituents has been little ... : Supplement to: Gieskes, Joris M; Lawrence, James R; Perry, Jr, Edward A; Grady, S J; Elderfield, Henry (1987): Chemistry of interstitial waters and sediments in the Norwegian-Greenland Sea, Deep Sea Drilling Project Leg 38. Chemical Geology, 63(1-2), 143-155 ... Dataset Greenland Greenland Sea Iceland DataCite Greenland
spellingShingle DEPTH, sediment/rock
Sample code/label
Sample type
Strontium-87/Strontium-86 ratio
Strontium-87/Strontium-86 ratio, error
Drilling/drill rig
DSDP/ODP/IODP sample designation
Leg38
Glomar Challenger
Deep Sea Drilling Project DSDP
Gieskes, Joris M
Lawrence, James R
Perry, Jr, Edward A
Grady, S J
Elderfield, Henry
(Table 2) 87Sr/86Sr ratios of DSDP Site 38-336 samples ...
title (Table 2) 87Sr/86Sr ratios of DSDP Site 38-336 samples ...
title_full (Table 2) 87Sr/86Sr ratios of DSDP Site 38-336 samples ...
title_fullStr (Table 2) 87Sr/86Sr ratios of DSDP Site 38-336 samples ...
title_full_unstemmed (Table 2) 87Sr/86Sr ratios of DSDP Site 38-336 samples ...
title_short (Table 2) 87Sr/86Sr ratios of DSDP Site 38-336 samples ...
title_sort (table 2) 87sr/86sr ratios of dsdp site 38-336 samples ...
topic DEPTH, sediment/rock
Sample code/label
Sample type
Strontium-87/Strontium-86 ratio
Strontium-87/Strontium-86 ratio, error
Drilling/drill rig
DSDP/ODP/IODP sample designation
Leg38
Glomar Challenger
Deep Sea Drilling Project DSDP
topic_facet DEPTH, sediment/rock
Sample code/label
Sample type
Strontium-87/Strontium-86 ratio
Strontium-87/Strontium-86 ratio, error
Drilling/drill rig
DSDP/ODP/IODP sample designation
Leg38
Glomar Challenger
Deep Sea Drilling Project DSDP
url https://dx.doi.org/10.1594/pangaea.705147
https://doi.pangaea.de/10.1594/PANGAEA.705147