Chemical composition and isotopic ratios of basic lavas from Iceland and the surrounding ocean floor ...

Major and trace dement data are used to establish the nature and extent of spatial and temporal chemical variations in basalts erupted in the Iceland region of the North Atlantic Ocean. The ocean floor samples are those recovered by legs 38 and 49 of the Deep Sea Drilling Project. Within each of the...

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Main Authors: Wood, D A, Joron, Jean Louis, Treuil, M, Norry, Michael J, Tarney, J
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1979
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.667460
https://doi.pangaea.de/10.1594/PANGAEA.667460
id ftdatacite:10.1594/pangaea.667460
record_format openpolar
spelling ftdatacite:10.1594/pangaea.667460 2024-09-15T18:13:15+00:00 Chemical composition and isotopic ratios of basic lavas from Iceland and the surrounding ocean floor ... Wood, D A Joron, Jean Louis Treuil, M Norry, Michael J Tarney, J 1979 application/zip https://dx.doi.org/10.1594/pangaea.667460 https://doi.pangaea.de/10.1594/PANGAEA.667460 en eng PANGAEA https://dx.doi.org/10.1007/bf00375360 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Multiple investigations Leg38 Leg49 Glomar Challenger Deep Sea Drilling Project DSDP article Collection Supplementary Publication Series of Datasets 1979 ftdatacite https://doi.org/10.1594/pangaea.66746010.1007/bf00375360 2024-08-01T10:59:11Z Major and trace dement data are used to establish the nature and extent of spatial and temporal chemical variations in basalts erupted in the Iceland region of the North Atlantic Ocean. The ocean floor samples are those recovered by legs 38 and 49 of the Deep Sea Drilling Project. Within each of the active zones on Iceland there are small scale variations in the light rare earth elements and ratios such as K/Y: several central complexes and their associated fissure swarms erupt basalts with values of K/Y distinct from those erupted at adjacent centres; also basalts showing a wide range of immobile trace element ratios occur together within single vertical sections and ocean floor drill holes. Although such variations can be explained in terms of the magmatic processes operating on Iceland they make extrapolations from single basalt samples to mantle sources underlying the outcrop of the sample highly tenuous. 87Sr/86Sr ratios measured for 25 of the samples indicate a total range from 0.7028 in a tholeiite ... : Supplement to: Wood, D A; Joron, Jean Louis; Treuil, M; Norry, Michael J; Tarney, J (1979): Elemental and Sr isotope variations in basic lavas from Iceland and the surrounding ocean floor. Contributions to Mineralogy and Petrology, 70(3), 319-339 ... Article in Journal/Newspaper Iceland North Atlantic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Multiple investigations
Leg38
Leg49
Glomar Challenger
Deep Sea Drilling Project DSDP
spellingShingle Drilling/drill rig
Multiple investigations
Leg38
Leg49
Glomar Challenger
Deep Sea Drilling Project DSDP
Wood, D A
Joron, Jean Louis
Treuil, M
Norry, Michael J
Tarney, J
Chemical composition and isotopic ratios of basic lavas from Iceland and the surrounding ocean floor ...
topic_facet Drilling/drill rig
Multiple investigations
Leg38
Leg49
Glomar Challenger
Deep Sea Drilling Project DSDP
description Major and trace dement data are used to establish the nature and extent of spatial and temporal chemical variations in basalts erupted in the Iceland region of the North Atlantic Ocean. The ocean floor samples are those recovered by legs 38 and 49 of the Deep Sea Drilling Project. Within each of the active zones on Iceland there are small scale variations in the light rare earth elements and ratios such as K/Y: several central complexes and their associated fissure swarms erupt basalts with values of K/Y distinct from those erupted at adjacent centres; also basalts showing a wide range of immobile trace element ratios occur together within single vertical sections and ocean floor drill holes. Although such variations can be explained in terms of the magmatic processes operating on Iceland they make extrapolations from single basalt samples to mantle sources underlying the outcrop of the sample highly tenuous. 87Sr/86Sr ratios measured for 25 of the samples indicate a total range from 0.7028 in a tholeiite ... : Supplement to: Wood, D A; Joron, Jean Louis; Treuil, M; Norry, Michael J; Tarney, J (1979): Elemental and Sr isotope variations in basic lavas from Iceland and the surrounding ocean floor. Contributions to Mineralogy and Petrology, 70(3), 319-339 ...
format Article in Journal/Newspaper
author Wood, D A
Joron, Jean Louis
Treuil, M
Norry, Michael J
Tarney, J
author_facet Wood, D A
Joron, Jean Louis
Treuil, M
Norry, Michael J
Tarney, J
author_sort Wood, D A
title Chemical composition and isotopic ratios of basic lavas from Iceland and the surrounding ocean floor ...
title_short Chemical composition and isotopic ratios of basic lavas from Iceland and the surrounding ocean floor ...
title_full Chemical composition and isotopic ratios of basic lavas from Iceland and the surrounding ocean floor ...
title_fullStr Chemical composition and isotopic ratios of basic lavas from Iceland and the surrounding ocean floor ...
title_full_unstemmed Chemical composition and isotopic ratios of basic lavas from Iceland and the surrounding ocean floor ...
title_sort chemical composition and isotopic ratios of basic lavas from iceland and the surrounding ocean floor ...
publisher PANGAEA
publishDate 1979
url https://dx.doi.org/10.1594/pangaea.667460
https://doi.pangaea.de/10.1594/PANGAEA.667460
genre Iceland
North Atlantic
genre_facet Iceland
North Atlantic
op_relation https://dx.doi.org/10.1007/bf00375360
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.66746010.1007/bf00375360
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