Helium isotopic composition of hydrothermal fluids from the Manus back-arc Basin, Papua New Guinea

We present isotopic analysis of helium in hydrothermal fluids from the Manus back-arc basin, collected during the French-Japanese Manusflux and Manaute cruises in 1995 and 2000, respectively. The helium isotope composition of the fluids is comparable to that measured elsewhere in similar subduction...

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Bibliographic Details
Published inGEOCHEMICAL JOURNAL Vol. 40; no. 3; pp. 245 - 252
Main Authors FOURRE, E., JEAN-BAPTISTE, P., CHARLOU, J.-L., DONVAL, J. P., ISHIBASHI, J. I.
Format Journal Article
LanguageEnglish
Published GEOCHEMICAL SOCIETY OF JAPAN 2006
The Geochemical Society of Japan
Subjects
back-arc basins
Continental interfaces, environment
helium isotopes
hydrothermal fluids
Manus Basin
Ocean, Atmosphere
Sciences of the Universe
western Pacific
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Summary:We present isotopic analysis of helium in hydrothermal fluids from the Manus back-arc basin, collected during the French-Japanese Manusflux and Manaute cruises in 1995 and 2000, respectively. The helium isotope composition of the fluids is comparable to that measured elsewhere in similar subduction environments, with 3He/4He values (7.4 to 7.9 Ra) slightly lower than typical MORB values, except on the Manus Spreading Center (MSC) where higher values (12 ± 0.1 Ra) are observed. The causal link between the narrow spatial extent of the 3He/4He anomaly at the MSC and a 3He-rich deep mantle component remains elusive, based on available geophysical data. Thus, the Manus Spreading Center results may be an interesting example of small scale upper-mantle heterogeneity.
ISSN:0016-7002
1880-5973
DOI:10.2343/geochemj.40.245