by
email: spearf@rpi.edu
Figure 2. Photomicrograph of pigeonite megacryst from sample AS-31. Note
reaction rim of clinopyroxene and orthopyroxene along top margin of crystal
and crystals of biotite and hornblende at the margin of the pyroxene cluster.
Matrix is plagioclase. Width of field is 17 mm.
Photomicrograph of approximately 1/2 of thin section
X-ray map: Xan in plagioclase
X-ray map: Fe/(Fe+Mg) in garnet (red), orthopyroxene (green) and clinopyroxene
(blue) (white is oxides)
Figure 3. Photomicrograph and X-ray composition maps from sample AS-31.
Note the core to rim decrease in Al and Fe/(Fe+Mg) and increase in Ca in
clinopyroxene and the absence of systematic Fe/(Fe+Mg) zoning in orthopyroxene.
Plagioclase shows increase in XAn towards the reaction zone. Field of view
in (a) is 4.4 mm.
Photomicrograph detail of metamorphic clino and orthopyroxene on margin
of pigeonite
X-ray map: Fe/(Fe+Mg) in clinopyroxene
X-ray map: Fe/(Fe+Mg) in orthopyroxene
X-ray map: Al in clinopyroxene
X-ray map: Ca in clinopyroxene
X-ray map: Xan in plagioclase
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