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Analytical method: ICPMS

TechniqueICPMS
MaterialWHOLE ROCK
Mineralnone
InstitutionMONASH UNIVERSITY
ReferenceGrove, T L; Parman, S W; Bowring, S A; Price, R C; Baker, M B (2002) The role of an H (sub 2) O-rich fluid component in the generation of primitive basaltic andesites and andesites from the Mt. Shasta region, N California. Contributions to Mineralogy and Petrology, vol.142, no.4, pp.375-396, Jan 2002

Samples analysed with this method

82-85, 82-95, 85-3, 85-59, 82-92a, 85-48b, 83-50, 83-58, 95-13, 82-91b, 83-54, 85-la, 95-15, 82-94a, 82-94d, 85-44, 85-41b, 85-38, 85-51