Publication | Closed Access
APPLICATION OF THE ICP‐MS TECHNIQUE TO TRACE ELEMENT ANALYSIS OF PERIDOTITES AND THEIR MINERALS
194
Citations
10
References
1992
Year
Rare Earth MineralMineral PhysicEngineeringTrace Element GeochemistryBiological Mass SpectrometryChemistryMineral ProcessingPlasma Mass SpectrometryAnalytical ChemistryElemental CharacterizationTrace ElementMaterials ScienceInorganic ChemistrySpark‐source Mass SpectrometryGeologyNatural SciencesThermal IonisationMass SpectrometryGeochemistryPetrologyMineral Geochemistry
Inductively coupled plasma mass spectrometry (ICP‐MS) has been applied to the determination of Rb, Sr, Ba, Zr, Hf, Nb, Ta, Th, U, Pb, Sc and 14 REE in peridotites and their constituent minerals: garnet, clinopyroxene, orthopyroxene and olivine. Determination limits for most elements are 1–10 ppb (in the solid sample), with accuracy and precision comparable to those of thermal ionisation and spark‐source mass spectrometry. New data on international standards PCC‐1, DTS‐1, UB‐N and JP‐1 are reported.
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