Petrogenetic relationship between mafic magma of somma lavas and voluminous felsic magma with caldera formation: A case study of Akan volcanic field, eastern Hokkaido, Japan
Author:
Affiliation:
1. Department of Earth Science, Hokkaido University of Education at Kushiro
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/97/2/97_2_39/_pdf
Reference21 articles.
1. Allègre, C.J. and Minster, J.F. (1978) Quantitative models of trace element behavior in magmatic processes. Earth and Planetary Science Letters, 38, 1-25.
2. Basaltic Volcanism Study Project (1981) Basaltic Volcanism on the Terrestrial Planets. pp. 1286, Pergamon Press Inc, New York.
3. Geological Survey of Hokkaido (1980) Geological map of Hokkaido, 1 : 600,000. Geological Survey of Hokkaido, Sapporo.
4. Gill, J. (1981) Orogenic Andesites and Plate Tectonics. pp. 385, Springer-Verlag, Berlin.
5. Hildreth, W. (1981) Gradients in silicic magma chamber: implications for lithospheric magmatism. Journal of Geophysical Research, 86, 10153-10192.
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1. Large scale explosive eruptions of Akan volcano, eastern Hokkaido, Japan: A geological and petrological case study for establishing tephro-stratigraphy and -chronology around a caldera cluster;Quaternary International;2016-03
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