@article{oai:nipr.repo.nii.ac.jp:00004673,
 author = {Miura, Yasunori and Iancu, Gabriel O. and Iancu, Gabriela and Yanai, Keizo and Haramura, Hiroshi},
 journal = {Proceedings of the NIPR Symposium on Antarctic Meteorites},
 month = {Mar},
 note = {P(論文), The Mocs meteorite, which fell on February 3,1882,in Transylvania over a large area (15km by 3km) has been reclassified from a L6 to a L5-6 chondrite in this study. Six fragments of the Mocs chondrite were observed by optical microscopy and measured using electron microprobe analyses and standard wet chemical analysis. Although the petrologic type of the 6 samples is almost the same, 2 fragments : Mocs-1 and Mocs-3 show heterogeneous features (opaque shock veins and melt pockets) due to different shock degrees (S-5 and S-4,respectively). Therefore the mean shock degree of the Mocs chondrite was found to be S3-5. The Tauti meteorite which fell in 1937 in Transylvania was previously classified as L6 chondrite using the bulk chemical analyses of H. SAVU (St. Cerc. Geol., 2 (IV), 272,1959) (A. L. GRAHAM; Meteoritics, 14,1,1979; A. L. GRAHAM et al.; Catalogue of Meteorites, London, British Museum, Natural History, 1985). The chemical compositions of olivines and orthopyroxenes determined by electron microprobe analysis, the bulk chemical analysis, along with textural characteristics classify Tauti shower as L6 chondrite with a shock degree of S-3.},
 pages = {153--166},
 title = {Reexamination of Mocs and Tauti chondritic meteorites: Classification with shock degree},
 volume = {8},
 year = {1995}
}