FN Archimer Export Format
PT J
TI Sr‐Nd‐Hf isotopes along the Pacific Antarctic Ridge from 41 to 53°S
BT 
AF HAMELIN, Cedric
   DOSSO, Laure
   HANAN, Barry
   BARRAT, Jean-Alix
   ONDREAS, Helene
AS 1:1;2:2;3:3;4:1;5:2;
FF 1:;2:;3:;4:;5:PDG-DOP-DCB-GM-LGM;
C1 UBO, IUEM, Lab Domaines Ocean, UMR 6538, F-29280 Plouzane, France.
   IFREMER, CNRS, UMR 6538, Lab Domaines Ocean, F-29280 Plouzane, France.
   San Diego State Univ, San Diego, CA 92182 USA.
C2 UBO, FRANCE
   IFREMER, FRANCE
   UNIV SAN DIEGO STATE, USA
SI BREST
SE PDG-DOP-DCB-GM-LGM
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-univ-france
   copubli-int-hors-europe
IF 3.505
TC 18
TU Centre national de la recherche scientifique
   Institut National de l'Information Géographique et Forestière
   Institut de physique du globe
   Institut de recherche pour le développement
   Institut français de recherche pour l'exploitation de la mer
   Service Hydrographique et Océanographique de la Marine
   Université Paris Diderot
   Université Pierre et Marie Curie
   Université de Bretagne Occidentale
   Université de Bretagne-Sud
   Université de La Réunion
UR https://archimer.ifremer.fr/doc/00004/11526/8123.pdf
LA English
DT Article
CR PACANTARCTIC
   PACANTARCTIC 2
BO L'Atalante
DE ;Pacific-Antarctic;depleted mantle;Sr-Nd-Hf isotopes
AB Major, trace element and Sr-Nd-Hf isotope data in basalts collected along the Pacific-Antarctic Ridge ( PAR) axis between 53 and 41 S, far from any hotspot influence, reveal tight coherent geochemical variations within the depleted MORB mantle. All samples are located below the Pacific reference line defining two sub-oceanic mantle domains on each side of the Easter microplate. The data extend the PAR 66-53 S field towards more radiogenic Sr (0.70264), less radiogenic Nd (epsilon = 7.7) and Hf (epsilon = 11.4) values. The along ridge geochemical variability is closely related to the morphological segmentation of the ridge. Anomalous geochemical features are attributed to the atypical morphology of two segments due to the presence of off-axis magmatism. The first order ridge discontinuity defined by the Menard transform fault separates two slightly different mantle domains, each with its own history.
PY 2010
PD MAY
SO Geophysical Research Letters
SN 0094-8276
PU American Geophysical Union
VL 37
IS L10303
UT 000277963200003
BP 1
EP 5
DI 10.1029/2010GL042979
ID 11526
ER

EF