Evidence for extreme mantle fractionation in early Archaean ultramafic rocks from northern Labrador
Samarium-neodymium isotope data for tectonically interleaved fragments of lithospheric mantle and meta-komatiite from the North Atlantic craton provide the first direct record of mantle differentiation before 3,800 Myr ago. The results confirm the magnitude of light-rare-earth-element depletion in t...
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ftnasantrs:oai:casi.ntrs.nasa.gov:19910038883 2023-05-15T17:30:47+02:00 Evidence for extreme mantle fractionation in early Archaean ultramafic rocks from northern Labrador Collerson, Kenneth D. Campbell, Lisa M. Weaver, Barry L. Palacz, Zenon A. Unclassified, Unlimited, Publicly available Jan 17, 1991 http://ntrs.nasa.gov/search.jsp?R=19910038883 unknown http://ntrs.nasa.gov/search.jsp?R=19910038883 Accession ID: 91A23506 Copyright Other Sources 46 Nature; 349; 209-214 1991 ftnasantrs 2012-02-15T18:57:14Z Samarium-neodymium isotope data for tectonically interleaved fragments of lithospheric mantle and meta-komatiite from the North Atlantic craton provide the first direct record of mantle differentiation before 3,800 Myr ago. The results confirm the magnitude of light-rare-earth-element depletion in the early mantle, and also its depleted neodymium isotope composition. The mantle fragments were able to retain these ancient geochemical signatures by virtue of having been tectonically incorporated in buoyant felsic crust, thus escaping recycling and homogenization by mantle convection. Other/Unknown Material North Atlantic NASA Technical Reports Server (NTRS) |
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46 Collerson, Kenneth D. Campbell, Lisa M. Weaver, Barry L. Palacz, Zenon A. Evidence for extreme mantle fractionation in early Archaean ultramafic rocks from northern Labrador |
topic_facet |
46 |
description |
Samarium-neodymium isotope data for tectonically interleaved fragments of lithospheric mantle and meta-komatiite from the North Atlantic craton provide the first direct record of mantle differentiation before 3,800 Myr ago. The results confirm the magnitude of light-rare-earth-element depletion in the early mantle, and also its depleted neodymium isotope composition. The mantle fragments were able to retain these ancient geochemical signatures by virtue of having been tectonically incorporated in buoyant felsic crust, thus escaping recycling and homogenization by mantle convection. |
format |
Other/Unknown Material |
author |
Collerson, Kenneth D. Campbell, Lisa M. Weaver, Barry L. Palacz, Zenon A. |
author_facet |
Collerson, Kenneth D. Campbell, Lisa M. Weaver, Barry L. Palacz, Zenon A. |
author_sort |
Collerson, Kenneth D. |
title |
Evidence for extreme mantle fractionation in early Archaean ultramafic rocks from northern Labrador |
title_short |
Evidence for extreme mantle fractionation in early Archaean ultramafic rocks from northern Labrador |
title_full |
Evidence for extreme mantle fractionation in early Archaean ultramafic rocks from northern Labrador |
title_fullStr |
Evidence for extreme mantle fractionation in early Archaean ultramafic rocks from northern Labrador |
title_full_unstemmed |
Evidence for extreme mantle fractionation in early Archaean ultramafic rocks from northern Labrador |
title_sort |
evidence for extreme mantle fractionation in early archaean ultramafic rocks from northern labrador |
publishDate |
1991 |
url |
http://ntrs.nasa.gov/search.jsp?R=19910038883 |
op_coverage |
Unclassified, Unlimited, Publicly available |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Other Sources |
op_relation |
http://ntrs.nasa.gov/search.jsp?R=19910038883 Accession ID: 91A23506 |
op_rights |
Copyright |
_version_ |
1766127792127213568 |