@article{oai:sucra.repo.nii.ac.jp:00016671,
 author = {竹村, 貴人 and 小田, 匡寛 and 鈴木, 健一郎},
 journal = {埼玉大学地域共同研究センター紀要, Report of Cooperative Research Center, Saitama University},
 month = {},
 note = {Microcracks-related fabric, determined using a stereological method, is represented quantitatively by means of the crack tensor introduced by, and brittle failure of granitic rock (Inada granite) is discussed based on the crack tensor analysis. Orientation of stress-induced microcracks doesn't change much during brittle failure, depending primarily on the orientation of pre-existing microcracks. Inelastic volumetric strain at failure decrease with increasing confining pressure due to the fact that crack opening is controlled by the confining pressure., text, application/pdf},
 pages = {62--69},
 title = {岩石の脆性破壊のモデル化に関する研究},
 volume = {3},
 year = {2003}
}