Petrogenesis of Oligocene to Miocene volcanic rocks from the Toyama basin of the SW Japan arc: Temporal change of arc volcanism during the back-arc spreading in the Japan Sea
Author:
Affiliation:
1. Graduate School of Science and Technology, Niigata University
2. Faculty of Science, Niigata University
3. Graduate School of Science and Engineering, Yamagata University
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/118/1/118_221219a/_pdf
Reference98 articles.
1. Arakawa, Y. and Shinmura, T. (1995) Nd-Sr isotopic and geochemical characteristics of two contrasting types of calc-alkaline plutons in the Hida belt, Japan. Chemical Geology, 124, 217-232.
2. Asano, M., Tanaka, T. and Suwa, K. (1990) Sm-Nd and Rb-Sr ages of the Hida metamorphic rocks in the Wada-gawa area, Toyama Prefecture. The Journal of the Geological Society of Japan, 96, 957-966 (in Japanese with English abstract).
3. Ayalew, D. and Ishiwatari, A. (2011) Comparison of rhyolites from continental rift, continental arc and oceanic island arc: Implication for the mechanism of silicic magma generation. Island Arc, 20, 78-93.
4. Barrat, J.A., Zanda, B., Moynier, F., Bollinger, C., et al (2012) Geochemistry of CI chondrites: Major and trace elements, and Cu and Zn isotopes. Geochimica et Cosmochimica Acta, 83, 79-92.
5. Bouvier, A., Vervoort, J.D. and Patchett, P.J. (2008) The Lu-Hf and Sm-Nd isotopic composition of CHUR: Constraints from unequilibrated chondrites and implications for the bulk composition of terrestrial planets. Earth and Planetary Science Letters, 273, 48-57.
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