A. Greig et al., TRACE-ELEMENT ZONING IN CLINOPYROXENES FROM SPINEL PERIDOTITE XENOLITHS, Nuclear instruments & methods in physics research. Section B, Beam interactions with materials and atoms, 75(1-4), 1993, pp. 411-414
The excellent spatial resolution of the proton microprobe allows trace
element zoning profiles to be determined within single grains of mant
le minerals. Analyses of clinopyroxenes from two spinel peridotite xen
oliths from the young basaltic volcanic field of the Western Districts
of Victoria show they have pronounced zoning in Ti, Zr and Sr. These
zoning profiles demonstrate that regions of the lithospheric mantle ha
ve undergone recent metasomatism by infiltrating basaltic melts result
ing in enrichment in Ti, Zr and Sr.