@article{oai:niigata-u.repo.nii.ac.jp:00028242,
 author = {茅原, 一也 and 青木, 滋 and 鈴木, 幸治},
 journal = {新潟大学積雪地域災害研究センター研究年報, 新潟大学積雪地域災害研究センター研究年報},
 month = {Mar},
 note = {1) The bed rocks in the Yoshiyama landslide area are mainly composed of the Pliocene deposits which are subdivided into the following formations (in descending order): Pliocene Eboshi-yama andesitic tuff breccia … Fault … Gray mudstone (2) The surface deposits in the studied area consist of the following sediments: a. Terrace deposits (T_1 ～ T_3) b. Talus breccia (Tcd) c. Landslide debris (Ld_1 ～ Ld_3) (3) The bed rock and surface geological map as shown in Fig. 2 represents a kind of mass-movement hazard map in this area.},
 pages = {75--84},
 title = {新潟県西頸城郡能生町芳山地すべり地の地質},
 volume = {1},
 year = {1979}
}