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 in | Gankō : Ganseki Kōbutsu Kōshō Gakkai shi Vol. 94; no. 9; pp. 315 - 328 |
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Main Authors | , , |
Format | Journal Article |
Language | English Japanese |
Published |
Japan Association of Mineralogical Sciences
01.09.1999
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Subjects | |
Online Access | Get full text |
ISSN | 0914-9783 1881-3275 |
DOI | 10.2465/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. |
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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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CitedBy_id | crossref_primary_10_1002_2014JB011781 crossref_primary_10_1139_e04_012 crossref_primary_10_1007_s00410_013_0850_0 crossref_primary_10_2465_jmps_071214 crossref_primary_10_2465_gkk_29_28 crossref_primary_10_1111_j_1440_1738_2005_00461_x crossref_primary_10_1111_j_1440_1738_2007_00566_x crossref_primary_10_2465_jmps_081011 |
Cites_doi | 10.1038/362144a0 10.1130/0091-7613(1986)14<848:CMOACG>2.0.CO;2 10.1111/j.1440-1738.1997.tb00042.x 10.1086/629737 10.1016/0040-1951(93)90276-P 10.1016/0040-1951(92)90296-I 10.5575/geosoc.88.271 10.1038/347662a0 10.1007/BF00372872 10.1130/0091-7613(1995)023<0395:SMAAEO>2.3.CO;2 10.1086/627519 10.2465/ganko1941.72.85 10.1007/BF00371501 10.1007/978-3-642-68012-0 10.2475/ajs.274.4.321 10.4294/zisin1948.38.2_193 10.1130/0091-7613(1993)021<0547:MSHPEO>2.3.CO;2 10.5575/geosoc.83.725 10.1086/648229 10.5026/jgeography.99.43 10.1016/S0012-821X(98)00041-7 10.1016/0377-0273(78)90032-X 10.2973/odp.proc.sr.131.103.1993 10.1016/S0016-7037(67)80031-0 |
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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. 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(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 doi: 10.1038/362144a0 – ident: 3 doi: 10.1130/0091-7613(1986)14<848:CMOACG>2.0.CO;2 – volume: 6 start-page: 91 issn: 1038-4871 issue: 1 year: 1997 ident: 16 doi: 10.1111/j.1440-1738.1997.tb00042.x – volume: 103 start-page: 213 issn: 0022-1376 issue: 2 year: 1995 ident: 6 doi: 10.1086/629737 – ident: 24 doi: 10.1016/0040-1951(93)90276-P – ident: 40 doi: 10.1016/0040-1951(92)90296-I – ident: 29 doi: 10.5575/geosoc.88.271 – ident: 12 – volume: 67 start-page: 1 issn: 0003-004X issue: 1/2 year: 1982 ident: 1 – ident: 37 – ident: 33 – ident: 10 – ident: 4 doi: 10.1038/347662a0 – ident: 34 doi: 10.1007/BF00372872 – ident: 28 – ident: 19 doi: 10.1130/0091-7613(1995)023<0395:SMAAEO>2.3.CO;2 – ident: 25 doi: 10.1086/627519 – ident: 31 doi: 10.2465/ganko1941.72.85 – ident: 9 – ident: 36 doi: 10.1007/BF00371501 – ident: 7 doi: 10.1007/978-3-642-68012-0 – ident: 20 – ident: 41 – ident: 17 – volume: 82 start-page: 1019 issn: 0003-004X issue: 9-10 year: 1997 ident: 15 – ident: 18 doi: 10.2475/ajs.274.4.321 – ident: 38 doi: 10.4294/zisin1948.38.2_193 – ident: 5 doi: 10.1130/0091-7613(1993)021<0547:MSHPEO>2.3.CO;2 – ident: 26 doi: 10.5575/geosoc.83.725 – volume: 101 start-page: 357 issn: 0022-1376 issue: 3 year: 1993 ident: 35 doi: 10.1086/648229 – ident: 13 – ident: 32 – ident: 11 doi: 10.5026/jgeography.99.43 – ident: 30 – ident: 39 doi: 10.1016/S0012-821X(98)00041-7 – ident: 14 doi: 10.1016/0377-0273(78)90032-X – ident: 22 doi: 10.2973/odp.proc.sr.131.103.1993 – ident: 21 – ident: 27 – ident: 8 doi: 10.1016/S0016-7037(67)80031-0 – ident: 23 |
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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 |
URI | https://www.jstage.jst.go.jp/article/ganko/94/9/94_9_315/_article/-char/en |
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