1963 年 50 巻 4 号 p. 135-141
Abstract: The basalts and andesites of the Ryozen formation (Miocene in age) of the northern Abukuma region, northeastern Japan are chemically analyzed. The aphyric basalts of the lower and upper parts of the formation are characterized by high Al2O3 content and their mineralogy and chemistry agree with that of the Kuno's high alumna basalt (Kuno, 1960). On the other hand, the olivine basalts of the middle part are relatively rich in MgO and poor in alkalies and TiO2, thus bear the character of the tholeiitic basalts.