Pyroxenite-rich mantle formed by recycled oceanic lithosphere: Oxygen-osmium isotope evidence from Canary Island lavas
Author:
Publisher
Geological Society of America
Subject
Geology
Link
http://pubs.geoscienceworld.org/geology/article-pdf/37/6/555/3537129/i0091-7613-37-6-555.pdf
Reference33 articles.
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3. Rheniumosmium isotope and elemental behaviour during subduction of oceanic crust and implications for mantle recycling:;Dale;Earth and Planetary Science Letters,2007
4. Inferences about magma sources and mantle structure variations in 143Nd/144Nd:;DePaolo;Geophysical Research Letters,1976
5. Oxygen isotope variations of basaltic lavas and upper mantle rocks:;Eiler;Reviews in Mineralogy and Geochemistry,2001
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