Evidence from10Be and U series disequilibria on the possible contamination of mid-ocean ridge basalt glasses by sedimentary material-Reference-Cited by-同舟云学术

Evidence from10Be and U series disequilibria on the possible contamination of mid-ocean ridge basalt glasses by sedimentary material

Published:2000-08 Issue:8 Volume:1 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Bourdon B.¹,Goldstein S. J.²,Bourlès D.³⁴,Murrell M. T.²,Langmuir C. H.⁵

Affiliation:

1. Laboratoire de Géochimie et Cosmochimie; CNRS-IPGP, T14-24; 4 Place Jussieu, F-75252 Paris Cedex 05 France

2. Los Alamos National Laboratory, J514; Los Alamos New Mexico 87545 USA

3. Centre de Spectrometrie Nucleaire et de Spectrometrie de Masse; IN2P3-CNRS, Bât. 104-108; F-91405 Orsay France

4. Centre Européan de Recherche et d'Enseignement de Géosciences de l'Environnement, BP 80; F-13545 Aix-en-Provence Cedex 04 France

5. Lamont-Doherty Earth Observatory of Columbia University; Palisades New York 10964 USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference28 articles.

1. Boundary scavenging in the Pacific Ocean: A comparison of 10Be and 231Pa;Anderson;Earth Planet. Sci. Lett.,1990

2. Constraints on mantle melting at mid-ocean ridges from global 238U-230Th disequilibrium data;Bourdon;Nature,1996

3. Ridge-hotspot interaction along the Mid-Atlantic Ridge between 37°30′ and 40°30′N: The U-Th disequilibrium evidence;Bourdon;Earth Planet. Sci. Lett.,1996

4. Bourlès , D. 1988 Etude de la géochimie de l'isotope 10 Be et de son isotope stable 9 Be en milieu océanique: Application à la datation des sédiments marins Paris-Sud, Orsay, France

5. Beryllium isotope geochemistry of hydrothermally altered sediments;Bourlès;Earth Planet. Sci. Lett.,1992

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