Major element, volatile, trace element and Sr-Nd-Hf-Pb isotope concentrations for basaltic glass samples from the Northern Lau Basin
Abstract:
Correction to the Cl data in Table S2 in Lytle et al., "Tracing mantle sources and Samoan influence in the northwestern Lau back-arc
basin" (G-Cubed, 2012). The Cl data measured at Carnegie Institution of Washington was found to have a significant interlaboratory bias of, on average, 23.9%. The Cl data was corrected by regressing a new calibration (using the new Cl values for the standards) against the measured SIMS 35Cl/30Si ratios, then taking the new slope as the calibration factor for your unknowns.
How to cite this dataset:
Lytle, M. L., Kelley, K. A., Hauri, E. H., Gill, J. B., Papia, D., Arculus, R. J., 2014. Major element, volatile, trace element and Sr-Nd-Hf-Pb isotope concentrations for basaltic glass samples from the Northern Lau Basin, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA).
https://doi.org/10.1594/IEDA/100419. Accessed 2024-04-25.
DOI Creation Date:
2014-01-14
Related
Publication(s):
Lytle, M. L., K. A. Kelley, E. H. Hauri, J. B. Gill, D. Papia, and R. J. Arculus (2012), Tracing mantle sources and Samoan influence in the northwestern Lau back-arc basin, Geochem. Geophys. Geosyst., 13, Q10019, doi:10.1029/2012GC004233.
License:
Creative Commons Attribution-NonCommercial-Share Alike 3.0 United States [CC-BY-NC-SA-3.0]
Keyword(s):
Coverage Scope: Regional (Continents, Oceans)
Geographic Location: Lau back-arc basin
User Contributed Keyword(s):
volatiles, major and trace elements, back-arc basin spreading centers, mantle heterogeneity, R2K (Ridge 2000) funded
Data Available On:
2014-01-15