Hi,

I don't understand the results I get from my EPMA calibrations.

When I analyze San carlos olivine as an unknown, I'm getting very good results and totals.

This is true when San Carlos olivine is used as a primary standard for Si and Mg (not very helpful).

This is ALSO true when Diopside is used as a primary standard for Si and Mg.

HOWEVER, when I analyze an olivine grain using the same analytical conditions (15kV, 20nA, focused beam) on a natural basalt sample I get a total of 97-98 wt%. (I analyse a large suite of elements: Na, Ca, ni, Mn, Ti, Al, Mg, Fe, Si, P, S, Cr, so there is no way there is a missing element) and by comparison with data from the literature, I can see Si (and to a lesser extent Mg) is underestimated. Analyses on BHVO also indicate an underestimation of SiO2.

I never had this issue before and I don't understand it. Any suggestions or tests I should do?

Thanks for the help.

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