Depleted mantle-plume geochemical signatures: No paradox for plume theories
High-MgO liquids erupted in ocean-island settings and in some continental flood-basalt provinces commonly preserve a "depleted" composition, in terms of both highly incompatible trace elements and isotope ratios. These observations strongly imply that their source is also compositionally d...
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1995
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ftunivcardiff:oai:https://orca.cardiff.ac.uk:9568 2023-05-15T16:50:06+02:00 Depleted mantle-plume geochemical signatures: No paradox for plume theories Kerr, Andrew Craig Saunders, A. D. Tarney, J. Berry, N. H. Hards, V. L. 1995-09 https://orca.cardiff.ac.uk/id/eprint/9568/ https://doi.org/10.1130/0091-7613(1995)0230843:DMPGSN2.3.CO;2 unknown Geological Society of America Kerr, Andrew Craig https://orca.cardiff.ac.uk/view/cardiffauthors/A0488436.html orcid:0000-0001-5569-4730 orcid:0000-0001-5569-4730, Saunders, A. D., Tarney, J., Berry, N. H. and Hards, V. L. 1995. Depleted mantle-plume geochemical signatures: No paradox for plume theories. Geology 23 (9) , pp. 843-846. 10.1130/0091-7613(1995)0230843:DMPGSN2.3.CO;2 https://doi.org/10.1130/0091-7613%281995%29023%3C0843%3ADMPGSN%3E2.3.CO%3B2 doi:10.1130/0091-7613(1995)0230843:DMPGSN2.3.CO;2 GC Oceanography QE Geology Article PeerReviewed 1995 ftunivcardiff https://doi.org/10.1130/0091-7613(1995)0230843:DMPGSN2.3.CO;2 2022-10-20T22:34:04Z High-MgO liquids erupted in ocean-island settings and in some continental flood-basalt provinces commonly preserve a "depleted" composition, in terms of both highly incompatible trace elements and isotope ratios. These observations strongly imply that their source is also compositionally depleted. However, in at least one case (Iceland and the North Atlantic volcanic province), it can be shown that this depleted source is not the same as that feeding the present-day North Atlantic mid-ocean ridge. The depleted source must also have been much hotter than the mid-ocean ridge basalt (MORB) source to account for the volume of melt and primitive composition of some magmas that were generated. This depleted character, then, is an intrinsic component of mantle plumes, originating from the deep mantle. We propose that mantle plumes consist of a mixture of enriched or fusible streaks in a depleted, refractory matrix; preferential extraction of the enriched component occurs close to the plume axis. The depleted residue from this melting remains in the upper mantle and may therefore be a major contributor to the source region of MORB. Article in Journal/Newspaper Iceland North Atlantic Ocean Island Cardiff University: ORCA (Online Research @ Cardiff) |
institution |
Open Polar |
collection |
Cardiff University: ORCA (Online Research @ Cardiff) |
op_collection_id |
ftunivcardiff |
language |
unknown |
topic |
GC Oceanography QE Geology |
spellingShingle |
GC Oceanography QE Geology Kerr, Andrew Craig Saunders, A. D. Tarney, J. Berry, N. H. Hards, V. L. Depleted mantle-plume geochemical signatures: No paradox for plume theories |
topic_facet |
GC Oceanography QE Geology |
description |
High-MgO liquids erupted in ocean-island settings and in some continental flood-basalt provinces commonly preserve a "depleted" composition, in terms of both highly incompatible trace elements and isotope ratios. These observations strongly imply that their source is also compositionally depleted. However, in at least one case (Iceland and the North Atlantic volcanic province), it can be shown that this depleted source is not the same as that feeding the present-day North Atlantic mid-ocean ridge. The depleted source must also have been much hotter than the mid-ocean ridge basalt (MORB) source to account for the volume of melt and primitive composition of some magmas that were generated. This depleted character, then, is an intrinsic component of mantle plumes, originating from the deep mantle. We propose that mantle plumes consist of a mixture of enriched or fusible streaks in a depleted, refractory matrix; preferential extraction of the enriched component occurs close to the plume axis. The depleted residue from this melting remains in the upper mantle and may therefore be a major contributor to the source region of MORB. |
format |
Article in Journal/Newspaper |
author |
Kerr, Andrew Craig Saunders, A. D. Tarney, J. Berry, N. H. Hards, V. L. |
author_facet |
Kerr, Andrew Craig Saunders, A. D. Tarney, J. Berry, N. H. Hards, V. L. |
author_sort |
Kerr, Andrew Craig |
title |
Depleted mantle-plume geochemical signatures: No paradox for plume theories |
title_short |
Depleted mantle-plume geochemical signatures: No paradox for plume theories |
title_full |
Depleted mantle-plume geochemical signatures: No paradox for plume theories |
title_fullStr |
Depleted mantle-plume geochemical signatures: No paradox for plume theories |
title_full_unstemmed |
Depleted mantle-plume geochemical signatures: No paradox for plume theories |
title_sort |
depleted mantle-plume geochemical signatures: no paradox for plume theories |
publisher |
Geological Society of America |
publishDate |
1995 |
url |
https://orca.cardiff.ac.uk/id/eprint/9568/ https://doi.org/10.1130/0091-7613(1995)0230843:DMPGSN2.3.CO;2 |
genre |
Iceland North Atlantic Ocean Island |
genre_facet |
Iceland North Atlantic Ocean Island |
op_relation |
Kerr, Andrew Craig https://orca.cardiff.ac.uk/view/cardiffauthors/A0488436.html orcid:0000-0001-5569-4730 orcid:0000-0001-5569-4730, Saunders, A. D., Tarney, J., Berry, N. H. and Hards, V. L. 1995. Depleted mantle-plume geochemical signatures: No paradox for plume theories. Geology 23 (9) , pp. 843-846. 10.1130/0091-7613(1995)0230843:DMPGSN2.3.CO;2 https://doi.org/10.1130/0091-7613%281995%29023%3C0843%3ADMPGSN%3E2.3.CO%3B2 doi:10.1130/0091-7613(1995)0230843:DMPGSN2.3.CO;2 |
op_doi |
https://doi.org/10.1130/0091-7613(1995)0230843:DMPGSN2.3.CO;2 |
_version_ |
1766040280116494336 |