@article{oai:u-ryukyu.repo.nii.ac.jp:02002271,
 author = {Hayashi, Daigoro and 林, 大五郎},
 issue = {38},
 journal = {琉球大学理学部紀要, Bulletin of the College of Science. University of the Ryukyus},
 note = {The Khaptar Gneiss Klippe, which occupies the northern part of the present region, constructs a successive western fringe of the Karnali Klippe. The area between this Klippe and the Dandeldhura Crystallines, which distribute in southern area of the region, is occupied by green mica schist (Doti Schist). The Dandeldhura Crystalline Massif are considered as eastern continuation of the Almora Nappe in Kumaun. The Doti Schist is doubtfully considered to be a member of the MCT zone in the region. The boundary between the Khaptar Gneiss and the underlying Doti Schist seems to be concordant., 紀要論文},
 pages = {103--116},
 title = {Geological reconnaissance around Silgarhi-Doti, West Central Nepal}
}