Magnetic Anomalies and the Corresponding Magnetic Centres. II
1950 年 2 巻 1 号 p. 25-28
詳細
1950 年 2 巻 1 号 p. 25-28
The method described in the first report is extended to cases in which magnetic anomalies are given in dip.
The changes in magnetic dip that accompanied the Shizuoka Earthquake of 1935 are studied as an example.
