敦賀(つるが)-大津(おおつ)ひずみ帶 : ひずみ帯における応用地質学的諸現象

概要

論文の詳細を見る
There is a distinct zonal distribution of land creeps, landslips, waste lands, and bare mountains from Tsuruga to Otsu along the west side of the Lake Biwa. These phenomenon will be caused by the presence of the geotectonic zone which is newly called Tsuruga-Otsu sheared zone by the writer. The presence of this zone is proved by many geological, geographical, and geophysical evidences.
地学団体研究会の論文
1956-10-31