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A young source for the Hawaiian plume.
Alexander V Sobolev1, Albrecht W Hofmann, Klaus Peter Jochum
1ISTerre, University Joseph Fourier, Grenoble 1 and CNRS, BP 53, 38041 Grenoble, France. alexander.sobolev@ujf-grenoble.fr
Ocean island volcanism involves recycling of oceanic crust. New strontium isotope data from Hawaiian lavas reveal seawater contamination, suggesting mantle circulation rates are faster than previously estimated.
Area of Science:
- Geochemistry
- Isotope Geochemistry
- Mantle Petrology
Background:
- Ocean island volcanism is explained by oceanic crust recycling via subduction and mantle plumes.
- Dating this recycling is crucial for understanding mantle circulation rates.
- Previous dating methods using lead and Re-Os isotopes have limitations due to mixing and rhenium mobility.
Purpose of the Study:
- To investigate the timescale of oceanic crust recycling in mantle plumes.
- To determine the age of subducted oceanic crust contributing to Hawaiian volcanism.
- To refine estimates of mantle circulation rates.
Main Methods:
- Analysis of strontium-87/strontium-86 ((87)Sr/(86)Sr) ratios in 138 melt inclusions from Mauna Loa olivine phenocrysts.
- Comparison of isotopic compositions with seawater and ancient crustal signatures.
- Modeling of isotopic data to infer source contamination and age.
Main Results:
- Enormous mantle source heterogeneity was identified in Mauna Loa lavas.
- Highly radiogenic strontium in depleted melt inclusions matches 200-650-million-year-old seawater.
- This indicates seawater contamination of the Mauna Loa source rock prior to subduction.
Conclusions:
- Seawater contamination provides a 'time stamp' for subducted oceanic crust.
- The presence of 200-650-million-year-old oceanic crust implies faster mantle circulation.
- Average mantle circulation rates are estimated at approximately 2 (±1) cm/yr, faster than previously thought.
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