XRF analysis of major and trace elements for wide compositional ranges from silicate rocks to carbonate rocks using low dilution glass beads

Japanese Magazine of Mineralogical and Petrological Sciences

Volumn 31, Issue 3, 2002, Pages 162-173

  Goto, Akiko ^a   Home, Taichiro ^a   Ohba, Tsukasa ^a   Fujimaki, Hirokazu ^a  

^a TOHOKU UNIVERSITY   (Japan)

Author keywords

Carbonate; Low dilution glass bead; Silicate; XRF

Indexed keywords

EID: 5444243540     PISSN: 1345630X     EISSN: 13497979     Source Type: Journal    
DOI: 10.2465/gkk.31.162     Document Type: Article

References (3)

1. Kimura J. and Yamada Y. (1996): Evaluation of major and trace element XRF analyses using a flux to sample ratio of two to one glass beads. J. Min. Petr. Econ. Geol., 91, 62–72.
2. Melezhik V.A., Gorokhov I.M., Fallick A.E. and Gjelle S. (2001): Strontium and carbon isotope geochemistry applied to dating of carbonate sedimentation: An example from high-grade rocks of the Norwegian Caledonides. Precambrian Research, 108, 267–292.
3. Norrish K. and Hutton J.T. (1969): An accurate X-ray spectrographs method for the analysis of a wide range of geochemical samples. Geochimi. Cosmochimi. Acta, 33, 431–453.