著者
応地 善雄
出版者
日本鉱物科学会
雑誌
岩石鉱物鉱床学会誌 (ISSN:00214825)
巻号頁・発行日
vol.45, no.4, pp.133-136, 1961

Phenocrystic olivine in picritic basalt from Mishima island and olivine in olivine nodule in trachybasalt from Tsukue island are chemically analysed and are expressed in following chemical formulas:<br> (Mg<sub>1.63</sub> Fe''<sub>0.30</sub> Fe<sub>0.06</sub>)<sub>1.99</sub> (Si<sub>0.98</sub> Ti<sub>0.01</sub>)<sub>0.99</sub> O<sub>4.00</sub><br> (Mg<sub>1.80</sub> Fe''<sub>0.14</sub> Fe<sub>0.05</sub>)<sub>1.99</sub> Si<sub>0.98</sub> O4.00<br> The former is distinctly richer in Fe than the latter. Such difference is attributed to their origin as already discussed by Ross and others.
著者
応地 善雄
出版者
日本鉱物科学会
雑誌
岩石鉱物鉱床学会誌 (ISSN:00214825)
巻号頁・発行日
vol.44, no.3, pp.129-141, 1960
被引用文献数
1

The Cenozoic volcanic rocks distributed in the Abu district, Yamaguchi Prefecture are divided into the following three groups from geologic relations and petrographic characters: 1) andesites and rhyolites of the calc-alkali rock series in Miocene age, 2) basalts of the tholeiitic series in Pliocene, 3) trachybasalts and trachyandesites of the alkali rock series, and andesites (so called quartz basalt) of the calc-alkali rock series in Quaternary. In this district, Quaternary trachybasalts, trachyandesites, and andesites are widely distributed contrasting to the other two groups. Of these, one of the second group and sixteen of the third are chemically analysed. Abundant quartz xenocrysts and granitic xenolithes are contained in some trachybasalts and trachyandesites, and in all andesites. On the other hand, it is notable that olivine nodules are included in some andesites. These facts are suggestive to consider that andesites are also to have derived from the alkali rock series by the contamination of granitic rocks as already pointed out by several petrologists.