@article{oai:nipr.repo.nii.ac.jp:00004648,
 author = {Ninagawa, Kiyotaka and Nakagawa, Masuo and Matoba, Atsuo and Yamaguchi, Hidetoshi and Yamamoto, Isao and Wada, Tomonori and Yamashita, Yoshihiko and Huang, Shaoxiong and Sears, Derek W.G. and Matsunami, Satoshi and Nishimura, Hiroshi},
 journal = {Proceedings of the NIPR Symposium on Antarctic Meteorites},
 month = {Mar},
 note = {P(論文), For most ordinary chondrites feldspar is mainly responsible for thermoluminescence [TL], but in type 3 ordinary chondrites, especially those which are most primitive, other minerals are important. We observed red TL with a ∿660nm spectral peak in an ordinary chondrite, Chainpur (LL3.4). The mineral responsible for the red TL was identified as iron-free enstatite. Spatial distribution of TL and cathodoluminescence [CL] for the same specimen was also investigated, and it was found that the red TL areas corresponded to the high-sensitivity areas of red CL.},
 pages = {217--224},
 title = {Red thermoluminescence of enstatite from the Chainpur meteorite},
 volume = {7},
 year = {1994}
}