Petrology of adakitic rocks from Quaternary Bishamon-dake volcano, central Japan

Quaternary Bishamon-dake volcano, central Japan, is composed of calc-alkalic clinopyroxene-orthopyroxene andesite and dacite with subordinate hornblende andesite having Sr/Y>40, SiO2 ∼63%, and Al2O3 ∼18%. The volcanic rocks are characteristically poorer in incompatible elements such as K2O and Rb...

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Published inGankō : Ganseki Kōbutsu Kōshō Gakkai shi Vol. 94; no. 9; pp. 315 - 328
Main Authors UJIKE, Osamu, WATANABE, Kazunori, TANAKA, Rumi
Format Journal Article
LanguageEnglish
Japanese
Published Japan Association of Mineralogical Sciences 01.09.1999
Subjects
Online AccessGet full text
ISSN0914-9783
1881-3275
DOI10.2465/ganko.94.315

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Abstract Quaternary Bishamon-dake volcano, central Japan, is composed of calc-alkalic clinopyroxene-orthopyroxene andesite and dacite with subordinate hornblende andesite having Sr/Y>40, SiO2 ∼63%, and Al2O3 ∼18%. The volcanic rocks are characteristically poorer in incompatible elements such as K2O and Rb than rocks from the adjacent volcanoes (Dainichi-dake, Eboshi and Washiga-take, Gankyoji, Haku-san, Kyoga-take, and Tomuro). They are essentially mixing products between two magmas; an andesite having SiO2 ∼60% and higher in FeO.t/MgO (FeO.t denotes total iron as FeO), and an adakite richer in SiO2 and lower in FeO.t/MgO carrying phenocrysts of orthopyroxene with Mg/(Mg+Fe) ∼0.80 and clinopyroxene with Mg/(Mg+Fe) ∼0.82 and presumed mantle-derived olivine (Fo ∼90) xenocrysts. The end-member andesite magma may have been formed by regional volcanism or lower crustal anatexis, while the end-member adakite magma is likely to have been locally generated beneath Bishamon-dake. The end-member adakite magma had SiO2>65%, Na2O≤3.2%, K2O≤1.2%, Rb≤20 ppm, Y<10 ppm, Nb≤6 ppm, FeO.t/MgO≤1.6 and Sr/Y>60, and was presumably generated by melting of the subducting Philippine Sea plate.
AbstractList Quaternary Bishamon-dake volcano, central Japan, is composed of calc-alkalic clinopyroxene-orthopyroxene andesite and dacite with subordinate hornblende andesite having Sr/Y>40, SiO2 ∼63%, and Al2O3 ∼18%. The volcanic rocks are characteristically poorer in incompatible elements such as K2O and Rb than rocks from the adjacent volcanoes (Dainichi-dake, Eboshi and Washiga-take, Gankyoji, Haku-san, Kyoga-take, and Tomuro). They are essentially mixing products between two magmas; an andesite having SiO2 ∼60% and higher in FeO.t/MgO (FeO.t denotes total iron as FeO), and an adakite richer in SiO2 and lower in FeO.t/MgO carrying phenocrysts of orthopyroxene with Mg/(Mg+Fe) ∼0.80 and clinopyroxene with Mg/(Mg+Fe) ∼0.82 and presumed mantle-derived olivine (Fo ∼90) xenocrysts. The end-member andesite magma may have been formed by regional volcanism or lower crustal anatexis, while the end-member adakite magma is likely to have been locally generated beneath Bishamon-dake. The end-member adakite magma had SiO2>65%, Na2O≤3.2%, K2O≤1.2%, Rb≤20 ppm, Y<10 ppm, Nb≤6 ppm, FeO.t/MgO≤1.6 and Sr/Y>60, and was presumably generated by melting of the subducting Philippine Sea plate.
Author WATANABE, Kazunori
UJIKE, Osamu
TANAKA, Rumi
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  fullname: WATANABE, Kazunori
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  fullname: TANAKA, Rumi
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10.1130/0091-7613(1986)14<848:CMOACG>2.0.CO;2
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10.5575/geosoc.88.271
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10.1130/0091-7613(1995)023<0395:SMAAEO>2.3.CO;2
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38
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39
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(35) 1993; 101
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2
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4
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7
8
(6) 1995; 103
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41
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21
References_xml – reference: Gill, J.B. (1981), Orogenic andesites and plate tectonics. pp. 390, Springer-Verlag, Berlin, Germany.
– reference: Wood, B.J. and Banno, S. (1973), Garnet-orthopyroxene and orthopyroxene-clinopyroxene relationships in simple and complex systems. Contrib. Mineral. Petrol., 42, 109-124.
– reference: Nagaoka, M. (1972), Geological and petrological study of Hakusan volcano. Master thesis, Kanazawa Univ., pp. 81 (in Japanese).*
– reference: Matsui, Y. and Nishizawa, O. (1974), Iron (II)-magnesium exchange equilibrium between olivine and calcium-free pyroxene over a temperature range 800°C to 1300°C. Bull. Soc. fr. Minéral. Crystallogr., 97, 122-130.
– reference: Hayami, K. (1981), Geology and petrology of Gankyoji volcano, southern part of the Ryohaku Mountains. Graduation thesis, Kanazawa Univ., pp. 50 (in Japanese).*
– reference: Tanase, A. (1982), Okumino Acid Igneous Complex —Cretaceous igneous activity in the Ryohaku Mountains, central Japan—. J. Geol. Soc. Japan, 88, 271-288 (in Japanese with English abstract).
– reference: Green, D.H. and Ringwood, A.E. (1967), An experimental investigation of the gabbro to eclogite transformation and its petrological applica-tions. Geochim. Cosmochim. Acta, 31, 767-833.
– reference: Suzuki, M. (1997), Petrology of eastern part of Eboshi-Washiga-take volcano. Master thesis, Toyama Univ., pp. 114 (in Japanese with English abstract).
– reference: Takahashi, E. (1986), Origin of basaltic magmas —Implications from peridotite melting experiments and an olivine fractionation model—. Bull. Volcanol. Soc. Japan, 30, S17-S40 (in Japanese with English abstract).
– reference: Obata, M., Banno, S. and Mori, T. (1974), The iron-magnesium partitioning between naturally occurring coexisting olivine and Ca-rich clinopyroxene: an application of the simple mixture model to olivine solid solution. Bull. Soc. fr. Minéral. Crystallogr., 97, 101-107.
– reference: Sakata, S., Higashino, T. and Yamasaki, M. (1992), Geology and petrology of Dainichiga-dake volcano in Central Japan. Res. Rept., Ishikawa Prefectural Nature Conservation Center of Hakusan, 19, 1-20 (in Japanese with English abstract).
– reference: Sugisaki, R., Shimomura, T., and Ando, K. (1977), An automatic X-ray fluorescence method for the analysis of silicate rocks. J. Geol. Soc. Japan, 83, 725-733 (in Japanese with English abstract).
– reference: Ujike, O. (1977), Chemical compositions of amphibole phenocrysts in calc-alkaline volcanic rocks: A compilation of 95 analyses. J. Japan. Assoc. Min. Petr. Econ. Geol., 72, 85-93 (in Japanese with English Abstract).
– reference: Terashima, S. (1977), X-ray fluorescence determination of chromium, gallium, niobium, lead, rubidium, strontium, yttrium, zinc and zirconium in rocks. Bull. Geol. Surv. Japan, 28, 393-399.
– reference: Wolf, M.B. and Wyllie, P.J. (1993), Garnet growth during amphibolite anatexis: Implications of a garnetiferous restite. J. Geol., 101, 357-373.
– reference: Zhao, D., Horiuchi, S. and Hasegawa, A. (1992), Seismic velocity structure of the crust beneath the Japan Islands. Tectonophys., 212, 289-301.
– reference: Ishida, M. (1990), Seismicity in the South Fossa Magna and the northern margin of the Philippine Sea plate. J. Geogr., 99, 43-60 (in Japanese with English abstract).
– reference: Yamaoka, K. and Nishihara, M. (1997), Geometry of subducting Philippine Sea plate and its relationship with the volcanism in Chubu district, Japan. Bull. Volcanol. Soc. Japan, 42, S131-S138 (in Japanese with English abstract).
– reference: Olafsson, G. (1993), Calcareous nannofossil biostratigraphy of the Nankai Trough. In Proc., Ocean Drilling Program, scientific results, (Hill, I.A., Taira, A., Firth, J.V., et al. Eds.), College Station, Texas., 131, 3-13.
– reference: Utsu, T. (1974), Epicenter distribution around Japan. Kagaku, 44, 739-746 (in Japanese).
– reference: Feeley, T.C. and Hacker, M.D. (1995), Intracrustal derivation of Na-rich andesitic and dacitic magmas: An example from Volcán Ollagüe, Andean Ventral Volcanic Zone. J. Geol., 103, 213-225.
– reference: Ikeda, T. (1986), Geology and petrology of Toritateyama volcanic rocks straddling the prefectural boundary of Ishikawa and Fukui. Graduation thesis, Kanazawa Univ., pp. 52 (in Japanese).*
– reference: Miyashiro, A. (1974), Volcanic rock series in island arcs and active continental margins. Amer. J. Sci., 274, 321-355.
– reference: Yogodzinski, G.M. and Kelemen, P.B. (1998), Slab melting in the Aleutians: implications of an ion probe study of clinopyroxene in primitive adakite and basalt. Earth Planet. Sci. Lett., 158, 53-65.
– reference: *appeared in Cenozoic volcanoes and volcanic rocks from Hokuriku District (Commemoration Committee for Retirement of Professor Masao Yamasaki, Ed.) (1988), pp. 155. Kanazawa University, Kanazawa (in Japanese).
– reference: Atherton, M.P. and Petford, N. (1993), Generation of sodium-rich magmas from newly underplated basaltic crust. Nature, 362, 144-146.
– reference: Iwasaki, E. (1981), Petrological study of Kyogadake volcano, Hokuriku. Master thesis, Kanazawa Univ., pp. 121 (in Japanese).*
– reference: Maruyama, S. (1997), Pacific-type orogeny revisited; Miyashiro-type orogeny proposed. Island Arc, 6, 91-120.
– reference: Yamazaki, F. and Ooida, T. (1985), Configuration of subducted Philippine Sea plate beneath the Chubu district, central Japan. Zishin, 38, 193-201 (in Japanese with English abstract).
– reference: Kay, R.W. (1978), Aleutian magnesian andesites: melts from subducted Pacific Ocean crust. J. Volcanol. Geotherm. Res., 4, 117-132.
– reference: Leake, B.E., Woolley, A.R., Arps, C.E.S., Birch, W.D., Gilbert, M.C., Grice, J.D., Hawthorne, F.C., Kato, A., Kisch, H.J., Krivovichev, V.G., Linthout, K., Laird, J., Mandarino, J.A., Maresch, W.V., Nickel, E.H., Rock, N.M.S., Schumacher, J.V., Smith, D.C., Stephenson, N.C.N., Ungaretti, L., Whittaker, E.J.W. and Youzhi, G. (1997), Nomenclature of amphiboles: Report of the Subcommittee on Amphiboles of the International Mineralogical Association, Commission on New Minerals and Mineral Names. Amer. Mineral., 82, 1019-1037.
– reference: Wells, P.R.A. (1997), Pyroxene geothermometry in simple and complex systems. Contrib. Mineral. Petrol., 62, 129-139.
– reference: Beard, J.S. (1986), Characteristic mineralogy of arc-related cumulate gabbros: Implications for the tectonic setting of gabbroic plutons and for andesite genesis. Geology, 14, 848-851.
– reference: Ujike, O. and Watanabe, K. (1994), Adakitic rocks from Bishamon-dake volcano, the Ryohaku Mountains, Central Japan. Program with abstracts, 1994 Japan Earth Planet. Sci. Joint Meeting, 383 (in Japanese).
– reference: Iwata, T. (1980), Geology and petrology of the northern part of Haku-san volcano. Graduation thesis, Kanazawa Univ., pp. 56 (in Japanese).*
– reference: Morris, P.A. (1995), Slab melting as an explanation of Quaternary volcanism and aseismicity in southwest Japan. Geology, 23, 395-398.
– reference: Simkin, T. and Smith, J.V. (1970), Minor element distribution in olivine. J. Geol., 78, 304-325.
– reference: Defant, M.J. and Drummond, M.S. (1993), Mount St. Helens: Potential example of the partial melting of the subducted lithosphere in a volcanic arc. Geology, 21, 547-550.
– reference: Shimizu, S. and Itaya, T. (1993), Plio-Pleistocene arc magmatism controlled by two overlapping subducted plates, central Japan. Tectonophys., 225, 139-154.
– reference: Aoki, K. and Fujimaki, H. (1982), Petrology and geochemistry of calc-alkaline andesite of presumed upper mantle origin from Itinome-gata, Japan. Amer. Mineral., 67, 1-13.
– reference: Defant, M.J. and Drummond, M.S. (1990), Derivation of modern arc magmas by melting of young subducted lithosphere. Nature, 347, 662-665.
– ident: 2
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Snippet Quaternary Bishamon-dake volcano, central Japan, is composed of calc-alkalic clinopyroxene-orthopyroxene andesite and dacite with subordinate hornblende...
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StartPage 315
SubjectTerms Adakite
Chemical composition
EPMA
Mantle olivine
Petrology
Philippine Sea plate
Slab melting
Title Petrology of adakitic rocks from Quaternary Bishamon-dake volcano, central Japan
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