posted on 2015-02-02, 16:21authored byT Noguchi, JC Bridges, Leon J. Hicks, Steven J. Gurman, M Kimura, T Hashimoto, M Konno, JP Bradley, R Okazaki, M Uesugi, T Yada, Y Karouji, M Abe, T Okada, T Mitsunari, T Nakamura, H Kagi
Four Itokawa particles collected from the first touchdown site were mineralogically investigated by optical microscopy,
micro-Raman (μ-Raman) spectrometry, scanning electron microscopy (SEM), electron microprobe analysis (EPMA), X-ray
absorption spectroscopy (XAS), and transmission electron microscopy (TEM). Their mineralogy has an affinity to that of
LL6 chondrites based on micro-Raman spectroscopy, EPMA, and XAS analyses. However, the space weathering rims on
them are less developed than those observed on the Itokawa particles collected from the second touchdown site. Solar
flare tracks are rarely observed in the four particles, whose number densities were lower than those observed in the
Itokawa particles from the second touchdown site.
Funding
J Bridges and L. Hicks were supported by STFC, UK
History
Citation
Noguchi et al.: Mineralogy of four Itokawa particles collected from the first touchdown site. Earth, Planets and Space 2014 66:124.
Author affiliation
/Organisation/COLLEGE OF SCIENCE AND ENGINEERING/Department of Physics and Astronomy
Version
VoR (Version of Record)
Published in
Noguchi et al.: Mineralogy of four Itokawa particles collected from the first touchdown site. Earth