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Petrology of Aoso volcano, northeast Japan arc: temporal variation of the magma feeding system and nature of low-K amphibole andesite in the Aoso-Osore volcanic zone

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Abstract

The Aoso volcano is a member of the newly defined volcanic front of Northeast Japan, characterized by the occurrence of low-K and hornblende andesites. Its activity can be divided into three stages: the early, caldera-forming, and late stages. While petrographic and geochemical data show all products underwent magma mixing or co-mingling, Sr and Nd isotopic ratios indicate that all are consanguineous. The end-member magmas are basaltic and andesitic in the early stage, but basaltic and dacitic in the late stage. In the caldera-forming stage, hornblende-free and hornblende-rich andesites co-mingled, which triggered an explosive eruption leading to caldera formation. Hornblende occurs also in the dacite from the early part of the late stage. These hornblende andesites and dacites are lower in magmatic temperature compared to hornblende-free andesites. The estimated basaltic end-member is low-K and high in magmatic temperature, and can be derived by a high degree of partial melting of mantle under the volcanic front. The estimated andesitic and dacitic end-members cannot be derived from the basaltic end-member magma through fractional crystallization, but can be derived from partial re-melting of the solidified low-K basalt, leaving amphibolitic and gabbroic residues, respectively.

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References

  • Ando S (1974) Geology and petrology of Esan volcano, Hokkaido, Japan (in Japanese with English abstract). J Jpn Assoc Miner Petrol Econ Geol 69:302–312

    CAS  Google Scholar 

  • Ban M, Yamamoto T (2002) Petrological study of Nasu-Chausudake volcano (ca. 16 ka to present), northeastern Japan. Bull Volcanol 64:100–116

    Article  Google Scholar 

  • Ban M, Oba Y, Ishikawa K and Takaoka N (1992) K–Ar dating of Mutsu-Hiuchidake, Osoreyama, Nanashigure, and Aoso volcanoes of the Aoso-Osore volcanic zone-The formation of the present volcanic zonation of the Northeast Japan arc (in Japanese with English abstract). J Miner Petrol Econ Geol 87:39–49

    CAS  Google Scholar 

  • Eichelberger JC (1980) Vesiculation of mafic magma during replenishment of silicic magma reservoirs. Nature 288:446–450

    CAS  Google Scholar 

  • Feeley TC, Dungan MA, Frey FA (1998) Geochemical constraints on the origin of mafic and silicic magmas at Cordon El Guadal, Tatara-San Pedro Complex, central Chile. Contrib Mineral Petrol 131:393–411

    Article  CAS  Google Scholar 

  • Fujinawa A (1988) Tholeiitic and calc-alkaline magma series at Adatara volcano, northeast Japan: 1. Geochemical constraints on their origin. Lithos 22:135–158

    Article  CAS  Google Scholar 

  • Fujinawa A (1991) Tholeiitic and calc-alkaline magma series at Adatara volcano, Northeast Japan: Evolution mechanism and genetic relationship (in Japanese with English abstract). Bull Volcanol Soc Jpn 36:241–254

    CAS  Google Scholar 

  • Gill JB (1981) Orogenic andesites and plate tectonics. Springer, Berlin Heidelberg New York

    Google Scholar 

  • Gust DA, Perfit MR (1987) Phase relations of high-Mg basalt from Aleutian island arc: implications for primary island arc basalts and high-Al basalts. Contrib Mineral Petrol 97:1–18

    Google Scholar 

  • Hansen J, Skjerlie KP, Pederson RB, Rosa JDL (2002) Crustal melting in the lower parts of island arcs: an example from the Bremanger Granitoid Complex, west Norwegian Caledonides. Contrib Mineral Petrol 143:316–335

    CAS  Google Scholar 

  • Hasenaka T, Aoki T (1995) Nanatsumori caldera and its model of formation (in Japanese). Res Rep Lab Geol Fukada, pp 155–173

    Google Scholar 

  • Hollister LS, Grissom GC, Peters EK, Stowell HH, Sisson VB (1987) Confirmation of the empirical correlation of Al in hornblende with pressure of solidification of calc-alkaline plutons. Am Mineral 72:231–239

    CAS  Google Scholar 

  • Inoue K, Ban M (1996) Petrology of younger stage lavas from the Gassan volcano, northeastern Japan (in Japanese with English abstract). J Miner Petrol Econ Geol 91:33–47

    CAS  Google Scholar 

  • Inoue M, Yoshida T, Fujimaki H, Ban M (1994) Geochemistry of Takahara volcano, northeastern Japan arc (in Japanese). Res Rep Lab Nuc Sci Tohoku Univ 25:199–226

    Article  CAS  Google Scholar 

  • Ishikawa K, Yoshida T, Kitagawa Y, Aoki K, Ogami K (1985) Geochemistry of Nanashigure volcano, Iwate Prefecture, northeastern Japan arc (in Japanese). Res Rep Lab Nuc Sci Tohoku Univ 18:366–378

    CAS  Google Scholar 

  • Johnson MC, Rutherford MJ (1989) Experimental calibration of the aluminum-in-hornblende geobarometer with application to Long Valley caldera (California) volcanic rocks. Geology 17:837–841

    Article  CAS  Google Scholar 

  • Kawamoto T (1992) Dusty and honeycomb plagioclase: indicators of processes in the Uchino stratified magma chamber, Izu Peninsula, Japan. J Volcanol Geotherm Res 29:413–450

    Google Scholar 

  • Kawano Y, Yagi K, Aoki K (1962) Petrography and petrochemistry of the volcanic rocks of Quaternary volcanoes of northeastern Japan. Sci Rep Tohoku Univ Ser III 7:1–46

    Google Scholar 

  • Kersting AB, Arculus RJ, Gust DA (1996) Lithospheric contributions to arc magmatism: Isotope variations along strike in volcanoes of Honshu, Japan. Science 272:1464–1468

    CAS  PubMed  Google Scholar 

  • Kouchi A, Sunagawa I (1985) A model for mixing of basaltic and dacitic magmas as deduced from experimental data. Contrib Mineral Petrol 89:17–23

    CAS  Google Scholar 

  • Kuno H (1966) Lateral variation of basalt magma type across continental margins and island arcs. Bull Volcanol 29:195–222

    CAS  Google Scholar 

  • Leak BE (1968) A catalogue of analyzed calciferous and subcalciferous amphiboles together with nomenclature and associated minerals. Geol Soc Amer Spec Pap 98:210

    Google Scholar 

  • Lindsley DH (1983) Pyroxene thermometry. Am Mineralogist 68:477–493

    CAS  Google Scholar 

  • Matsuda T, Ban M and Ohba Y (1997) Petrological characteristics of two types of inclusions and their host rocks from the Yudonosan volcano, southern part of the Chokai zone, northeast Japan (in Japanese with English abstract). J Miner Petrol Econ Geol 92:245–259

    CAS  Google Scholar 

  • Matsui Y, 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 Mineral Cristallogr 97:122–130

    Google Scholar 

  • Miyashiro A (1974) Volcanic rock series in island arcs and active continental margins. Am J Sci 274:321–355

    CAS  Google Scholar 

  • Murata M (1993) Major and trace elements analysis of Korea Institute of Energy and Resources igneous rock reference samples using X-ray fluorescence spectrometer (in Japanese with English abstract). J Naruto Coll Edue 8:37–50

    Google Scholar 

  • Nakagawa M (1991) Models for the generation of andesitic-dacitic magma of Moriyoshi volcano, Northeastern Japan (in Japanese with English abstract). Bull Volcanol Soc Jpn 36:223–239

    CAS  Google Scholar 

  • Nakagawa M, Shimotori H, Yoshida T (1986) Aoso-Osore volcanic zone—the volcanic front of the Northeast Honshu arc, Japan- (in Japanese with English abstract). J Miner Petrol Econ Geol 81:471–478

    Google Scholar 

  • Nakagawa M, Shimotori H, Yoshida T (1988) Across-arc compositional variation of the Quaternary basaltic rocks from the Northeast Japan arc (in Japanese with English abstract). J Miner Petrol Econ Geol 83:9–25

    CAS  Google Scholar 

  • Obata M, Banno S, 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 Mineral Cristallogr 97:101–107

    CAS  Google Scholar 

  • Ohba T, Umeda K (1999) Geology of Hachimantai volcanic field and temporal-spatial variation of the magma compositions (in Japanese with English abstract). J Miner Petrol Econ Geol 94:187–202

    CAS  Google Scholar 

  • Presnell DC, Dixon SA, Dixon JR, O’Donnell TH, Brenner NL, Schrock RL, Dycus DW (1978) Liquidus phase relations on the join diopside–forsterite–anorthite from 1 atm to 20 kb: their bearing on the generation and crystallization of basaltic magma. Contrib Mineral Petrol 66:203–220

    Google Scholar 

  • Rollinson H (1993) Using geochemical data: evaluation, presentation, interpretation. Longman Scientific and Technical, Harlow

    Google Scholar 

  • Sakayori A (1991) Magmatic evolution of Zao volcano, Northeast Japan (in Japanese with English abstract). Bull Volcanol Soc Jpn 36:79–92

    CAS  Google Scholar 

  • Sakuyama M, Nesbitt RW (1983) Geochemistry of the Quaternary volcanic rocks of the Northeast Japan arc. J Volcanol Geotherm Res 29:413–450

    Article  Google Scholar 

  • Shibata T, Nakamura E (1997) Across-arc variations of isotope and trace element compositions from Quaternary basaltic volcanic rock in northeastern Japan: implications for interaction between subducted oceanic slab and mantle wedge. J Geophys Res 102:8051–8064

    Article  CAS  Google Scholar 

  • Stormer JC Jr (1983) The effects of recalculation on estimates of temperature and oxygen fugacity from analyses of multicomponent iron-titanium oxides. Am Mineral 68:586–594

    CAS  Google Scholar 

  • Sugawara T (2000) Prediction of chemical compositions of olivine+plagioclase saturated magma (in Japanese). Volcanol Soc Jpn Fall meeting, abstract

  • Tatsumi Y (2003) High-Mg andesite genesis, continental crust formation, and mantle evolution (in Japanese). University of Tokyo Press, Tokyo

    Google Scholar 

  • Tatsumi Y, Eggins S (1995) Subduction zone magmatism. Blackwell, Oxford

    Google Scholar 

  • Tatsumi Y, Sakuyama M, Fukuyama H, Kushiro I (1983) Generation of arc magmas and thermal structure of the mantle wedge in subduction zones. J Geophys Res 88:5815–5825

    CAS  Google Scholar 

  • Togashi S (1977) Petrology of Osore-yama volcano, Japan (in Japanese with English abstract). J Jpn Assoc Miner Petrol Econ Geol 72:45–60

    CAS  Google Scholar 

  • Togashi S, Tanaka T, Yoshida T, Ishikawa K, Fujinawa A and Kurasawa H (1992) Trace elements and Nd–Sr isotopes of island arc tholeiites from frontal arc of northeast Japan. Geochem J 26:261–277

    CAS  Google Scholar 

  • Tomiya A (1995) Does the Usu volcano continue to erupt (in Japanese). Iwanami-Kagaku 67:692–697

    Google Scholar 

  • Toya N, Ban M (2001) Volcanic history and major element bulk chemistry of the Aoso volcano, Northeast Japan arc (in Japanese with English abstract). Jpn Mag Mineral Petrol Sci 30:105–116

    CAS  Google Scholar 

  • Toya N, Ban M, Ishikawa K, Kanisawa S (2001) Fluorine contents of rocks from Aoso volcano, Northeast Japan arc. Bull Volcanol Soc Jpn 46:335–341

    CAS  Google Scholar 

  • Tsuchiyama A (1985) Dissolution kinetics of plagioclase in the melt of the system diopside-albite-anorthite, and origin of dusty plagioclase in andesites. Contrib Mineral Petrol 89:1–16

    CAS  Google Scholar 

  • Ujike O (1988) Probable mineralogic control on the mantle metasomatic fluid composition beneath the northeast Japan arc. Geochim Cosmochim Acta 52:2037–2046

    Article  CAS  Google Scholar 

  • Wada K (1981) Contrasted petrological relations between tholeiitic and calc-alkalic series from Funagata volcano, northeast Japan. J Miner Petrol Econ Geol 76:215–232

    CAS  Google Scholar 

  • Yamada Y, Kohno H, Murata M (1995) A low dilution fusion method for major and trace element analysis of geological samples (in Japanese with English abstract). Advan X-ray anal 26:33–44

    Google Scholar 

  • Yoshinaga T, Nakagawa M (1999) Finding of primary basalt from Sannome-gata volcano, northeastern Japan, and its compositional variation (in Japanese with English abstract). J Miner Petrol Econ Geol 94:241–253

    CAS  Google Scholar 

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Acknowledgments

We are grateful to R.W. Jordan of Yamagata University for correcting the English in this paper. Many constructive comments and suggestions from anonymous reviewers and the editor T.L. Grove greatly helped to revise the manuscript. We also express our thanks to S. Kanisawa, H. Tanaka and K. Saito of Yamagata University for their continual support of this research. The constructive comments from T. Yoshida and M. Nakamura of Tohoku University, Y. Tatsumi and Y. Tamura of IFREE were helpful to complete this manuscript. We are grateful to S. Ohde of Ryukyus University for facility of isotope analyses. Parts of this study were supported by the Grants-in-Aid for Scientific Research from the Ministry of Education, Culture, Sports, Science and Technology, Japan (No. 13640483 to R. Shinjo).

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Toya, N., Ban, M. & Shinjo, R. Petrology of Aoso volcano, northeast Japan arc: temporal variation of the magma feeding system and nature of low-K amphibole andesite in the Aoso-Osore volcanic zone. Contrib Mineral Petrol 148, 566–581 (2005). https://doi.org/10.1007/s00410-004-0621-z

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