Figure 6
From: Mineralogy of four Itokawa particles collected from the first touchdown site
![Figure 6](http://media.springernature.com/full/springer-static/image/art%3A10.1186%2F1880-5981-66-124/MediaObjects/40623_2014_Article_115_Fig6_HTML.jpg)
Fe K-edge XANES spectra. (a) Fe K-edge of olivine in the three Itokawa particles: RB-QD04-0008, RB-QD04-0011, and RB-QD04-0015. Those of olivine in the Tuxtuac LL5 chondrite and San Carlos olivine are also plotted for comparison. (b) Fe K-edge of low-Ca pyroxene in RB-QD04-0024 and the Tuxtuac LL5 chondrite.