Geochemistry of North Atlantic Igneous Province basalts ...
New Sr-Nd-Pb-Hf data require the existence of at least four mantle components in the genesis of basalts from the the North Atlantic Igneous Province (NAIP): (1) one (or more likely a small range of) enriched component(s) within the Iceland plume, (2) a depleted component within the Iceland plume (di...
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ftdatacite:10.1594/pangaea.716921 2024-09-15T18:09:59+00:00 Geochemistry of North Atlantic Igneous Province basalts ... Kempton, Pamela D Fitton, J Godfrey Saunders, Andrew D Nowell, G M Taylor, R N Hardarson, B S Pearson, Grant 2000 application/zip https://dx.doi.org/10.1594/pangaea.716921 https://doi.pangaea.de/10.1594/PANGAEA.716921 en eng PANGAEA https://dx.doi.org/10.1016/s0012-821x(00)00047-9 https://dx.doi.org/10.1016/s0009-2541(98)00036-9 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg38 Leg49 Leg80 Leg81 Leg152 Leg163 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 2000 ftdatacite https://doi.org/10.1594/pangaea.71692110.1016/s0012-821x(00)00047-910.1016/s0009-2541(98)00036-9 2024-08-01T10:53:02Z New Sr-Nd-Pb-Hf data require the existence of at least four mantle components in the genesis of basalts from the the North Atlantic Igneous Province (NAIP): (1) one (or more likely a small range of) enriched component(s) within the Iceland plume, (2) a depleted component within the Iceland plume (distinct from the shallow N-MORB source), (3) a depleted sheath surrounding the plume and (4) shallow N-MORB source mantle. These components have been available since the major phase of igneous activity associated with plume head impact during Paleogene times. In Hf-Nd isotope space, samples from Iceland, DSDP Leg 49 (Sites 407, 408 and 409), ODP Legs 152 and 163 (southeast Greenland margin), the Reykjanes Ridge, Kolbeinsey Ridge and DSDP Leg 38 (Site 348) define fields that are oblique to the main ocean island basalt array and extend toward a component with higher 176Hf/177Hf than the N-MORB source available prior to arrival of the plume, as indicated by the compositions of Cretaceous basalts from Goban Spur (~95 ... : Supplement to: Kempton, Pamela D; Fitton, J Godfrey; Saunders, Andrew D; Nowell, G M; Taylor, R N; Hardarson, B S; Pearson, Grant (2000): The Iceland plume in space and time: a Sr-Nd-Pb-Hf study of the North Atlantic rifted margin. Earth and Planetary Science Letters, 177(3-4), 255-271 ... Article in Journal/Newspaper Greenland Iceland Kolbeinsey North Atlantic Ocean Island DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Drilling/drill rig Leg38 Leg49 Leg80 Leg81 Leg152 Leg163 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP |
spellingShingle |
Drilling/drill rig Leg38 Leg49 Leg80 Leg81 Leg152 Leg163 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP Kempton, Pamela D Fitton, J Godfrey Saunders, Andrew D Nowell, G M Taylor, R N Hardarson, B S Pearson, Grant Geochemistry of North Atlantic Igneous Province basalts ... |
topic_facet |
Drilling/drill rig Leg38 Leg49 Leg80 Leg81 Leg152 Leg163 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP |
description |
New Sr-Nd-Pb-Hf data require the existence of at least four mantle components in the genesis of basalts from the the North Atlantic Igneous Province (NAIP): (1) one (or more likely a small range of) enriched component(s) within the Iceland plume, (2) a depleted component within the Iceland plume (distinct from the shallow N-MORB source), (3) a depleted sheath surrounding the plume and (4) shallow N-MORB source mantle. These components have been available since the major phase of igneous activity associated with plume head impact during Paleogene times. In Hf-Nd isotope space, samples from Iceland, DSDP Leg 49 (Sites 407, 408 and 409), ODP Legs 152 and 163 (southeast Greenland margin), the Reykjanes Ridge, Kolbeinsey Ridge and DSDP Leg 38 (Site 348) define fields that are oblique to the main ocean island basalt array and extend toward a component with higher 176Hf/177Hf than the N-MORB source available prior to arrival of the plume, as indicated by the compositions of Cretaceous basalts from Goban Spur (~95 ... : Supplement to: Kempton, Pamela D; Fitton, J Godfrey; Saunders, Andrew D; Nowell, G M; Taylor, R N; Hardarson, B S; Pearson, Grant (2000): The Iceland plume in space and time: a Sr-Nd-Pb-Hf study of the North Atlantic rifted margin. Earth and Planetary Science Letters, 177(3-4), 255-271 ... |
format |
Article in Journal/Newspaper |
author |
Kempton, Pamela D Fitton, J Godfrey Saunders, Andrew D Nowell, G M Taylor, R N Hardarson, B S Pearson, Grant |
author_facet |
Kempton, Pamela D Fitton, J Godfrey Saunders, Andrew D Nowell, G M Taylor, R N Hardarson, B S Pearson, Grant |
author_sort |
Kempton, Pamela D |
title |
Geochemistry of North Atlantic Igneous Province basalts ... |
title_short |
Geochemistry of North Atlantic Igneous Province basalts ... |
title_full |
Geochemistry of North Atlantic Igneous Province basalts ... |
title_fullStr |
Geochemistry of North Atlantic Igneous Province basalts ... |
title_full_unstemmed |
Geochemistry of North Atlantic Igneous Province basalts ... |
title_sort |
geochemistry of north atlantic igneous province basalts ... |
publisher |
PANGAEA |
publishDate |
2000 |
url |
https://dx.doi.org/10.1594/pangaea.716921 https://doi.pangaea.de/10.1594/PANGAEA.716921 |
genre |
Greenland Iceland Kolbeinsey North Atlantic Ocean Island |
genre_facet |
Greenland Iceland Kolbeinsey North Atlantic Ocean Island |
op_relation |
https://dx.doi.org/10.1016/s0012-821x(00)00047-9 https://dx.doi.org/10.1016/s0009-2541(98)00036-9 |
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.71692110.1016/s0012-821x(00)00047-910.1016/s0009-2541(98)00036-9 |
_version_ |
1810447580964847616 |