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- W2321813181 startingPage "111" @default.
- W2321813181 abstract "Abstract: The Ryoke plutonic rocks of the Takato district have been divided into two groups, older and younger. The Hiji quartz dioritic rocks belonging to the older Ryoke plutonic rocks consist of amphibolites, fine to medium grained biotite-hornblende quartz diorites, biotite-hornblende granodiorites and aplitic granites. They have the different characteristics from the older Ryoke plutonic rocks of the other districts. Namely, in spite of the various rock types of the Hiji quartz dioritic rocks, hornblende, plagioclase and epidote in them show nearly invariable petrogenetical characteristics. Normative wollastonite is calculated from the chemical composition of the Hiji quartz dioritic rocks. These facts suggest that the Hiji quartz dioritic rocks have resulted from the granitization process of basic rocks in the condition of the lower-grade of amphibolite facies. In the mylonitization process of the Hiji quartz dioritic rocks, CaO decreases and Na2O increases. The petrological characters of the Osafuji quartz diorite are similar to those of the younger Ryoke plutonic rocks of the other districts." @default.
- W2321813181 created "2016-06-24" @default.
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- W2321813181 date "1961-01-01" @default.
- W2321813181 modified "2023-09-25" @default.
- W2321813181 title "Ryoke plutonic rocks of Takato district, Nagano Prefecture" @default.
- W2321813181 cites W3033994668 @default.
- W2321813181 doi "https://doi.org/10.2465/ganko1941.46.111" @default.
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