All Outputs (2)

Pyroxenite-rich mantle formed by recycled oceanic lithosphere: Oxygen-osmium isotope evidence from Canary Island lavas (2009)
Journal Article
Day, J., Pearson, D., Macpherson, C., Lowry, D., & Carracedo, J. (2009). Pyroxenite-rich mantle formed by recycled oceanic lithosphere: Oxygen-osmium isotope evidence from Canary Island lavas. Geology, 37(6), 555-558. https://doi.org/10.1130/g25613a.1

Plate tectonic processes result in recycling of crust and lithosphere into Earth's mantle. Evidence for long-term preservation of recycled reservoirs in the mantle comes from the enriched isotopic character of oceanic island basalt (OIB) lavas. Altho... Read More about Pyroxenite-rich mantle formed by recycled oceanic lithosphere: Oxygen-osmium isotope evidence from Canary Island lavas.

Community diversity at Ban Lum Khao, Thailand: Isotopic evidence from the skeletons (2009)
Journal Article
Bentley, R., Cox, K., Tayles, N., Higham, C., Macpherson, C., Nowell, G., …Hayes, T. (2009). Community diversity at Ban Lum Khao, Thailand: Isotopic evidence from the skeletons. Asian Perspectives: The Journal of Archaeology for Asia and the Pacific, 48(1), 79-97. https://doi.org/10.1353/asi.0.0017

Isotopes of strontium, carbon, and oxygen were analyzed in human tooth enamel from the Bronze Age site of Ban Lum Khao (c. 1400 B.C.–500 B.C.) in Thailand. The strontium and oxygen isotopes, which generally reflect place of origin, delimit discrete g... Read More about Community diversity at Ban Lum Khao, Thailand: Isotopic evidence from the skeletons.