Origin of felsic volcanism in the Izu arc intra-arc rift

Satoru Haraguchi, Jun Ichi Kimura, Ryoko Senda, Koichiro Fujinaga, Kentaro Nakamura, Yutaro Takaya, Teruaki Ishii

    Research output: Contribution to journalArticle

    5 Citations (Scopus)

    Abstract

    An intra-arc rift (IAR) is developed behind the volcanic front in the Izu arc, Japan. Bimodal volcanism, represented by basalt and rhyolite lavas and hydrothermal activity, is active in the IAR. The constituent minerals in the rhyolite lavas are mainly plagioclase and quartz, whereas mafic minerals are rare and are mainly orthopyroxene without any hydrous minerals such as amphibole and biotite. Both the phenocryst and groundmass minerals have felsic affinities with a narrow compositional range. The petrological and bulk chemical characteristics are similar to those of melts from some partial melting experiments that also yield dry rhyolite melts. The hydrous mineral-free narrow mineral compositions and low-Al2O3 affinities of the IAR rhyolites are produced from basaltic middle crust under anhydrous low-temperature melting conditions. The IAR basalt lavas display prominent across-arc variation, with depleted elemental compositions in the volcanic front side and enriched compositions in the rear-arc side. The across-arc variation reflects gradual change in the slab-derived components, as demonstrated by decreasing Ba/Zr and Th/Zr values to the rear-arc side. Rhyolite lavas exhibit different across-arc variations in either the fluid-mobile elements or the immobile elements, such as Nb/Zr, La/Yb, and chondrite-normalized rare earth element patterns, reflecting that the felsic magmas had different source. The preexisting arc crust formed during an earlier stage of arc evolution, most probably during the Oligocene prior to spreading of the Shikoku back-arc basin. The lack of systematic across-arc variation in the IAR rhyolites and their dry/shallow crustal melting origin combines to suggest re-melting of preexisting Oligocene middle crust by heat from the young basaltic magmatism.

    Original languageEnglish
    Article number25
    JournalContributions to Mineralogy and Petrology
    Volume172
    Issue number5
    DOIs
    Publication statusPublished - 2017 May 1

    Fingerprint

    rhyolite
    Minerals
    volcanism
    arcs
    hydrous mineral
    melting
    mineral
    crust
    Oligocene
    Melting
    basalt
    melt
    phenocryst
    minerals
    hydrothermal activity
    Amphibole Asbestos
    Chemical analysis
    orthopyroxene
    chondrite
    amphibole

    Keywords

    • Across-arc geochemical variation
    • Bimodal volcanism
    • Intra-arc rifting
    • Izu arc
    • Mantle-derived basalt
    • Rhyolite crustal melt

    ASJC Scopus subject areas

    • Geophysics
    • Geochemistry and Petrology

    Cite this

    Haraguchi, S., Kimura, J. I., Senda, R., Fujinaga, K., Nakamura, K., Takaya, Y., & Ishii, T. (2017). Origin of felsic volcanism in the Izu arc intra-arc rift. Contributions to Mineralogy and Petrology, 172(5), [25]. https://doi.org/10.1007/s00410-017-1345-1

    Origin of felsic volcanism in the Izu arc intra-arc rift. / Haraguchi, Satoru; Kimura, Jun Ichi; Senda, Ryoko; Fujinaga, Koichiro; Nakamura, Kentaro; Takaya, Yutaro; Ishii, Teruaki.

    In: Contributions to Mineralogy and Petrology, Vol. 172, No. 5, 25, 01.05.2017.

    Research output: Contribution to journalArticle

    Haraguchi, S, Kimura, JI, Senda, R, Fujinaga, K, Nakamura, K, Takaya, Y & Ishii, T 2017, 'Origin of felsic volcanism in the Izu arc intra-arc rift', Contributions to Mineralogy and Petrology, vol. 172, no. 5, 25. https://doi.org/10.1007/s00410-017-1345-1
    Haraguchi, Satoru ; Kimura, Jun Ichi ; Senda, Ryoko ; Fujinaga, Koichiro ; Nakamura, Kentaro ; Takaya, Yutaro ; Ishii, Teruaki. / Origin of felsic volcanism in the Izu arc intra-arc rift. In: Contributions to Mineralogy and Petrology. 2017 ; Vol. 172, No. 5.
    @article{13d0a05d13a94d36b7da93860f884757,
    title = "Origin of felsic volcanism in the Izu arc intra-arc rift",
    abstract = "An intra-arc rift (IAR) is developed behind the volcanic front in the Izu arc, Japan. Bimodal volcanism, represented by basalt and rhyolite lavas and hydrothermal activity, is active in the IAR. The constituent minerals in the rhyolite lavas are mainly plagioclase and quartz, whereas mafic minerals are rare and are mainly orthopyroxene without any hydrous minerals such as amphibole and biotite. Both the phenocryst and groundmass minerals have felsic affinities with a narrow compositional range. The petrological and bulk chemical characteristics are similar to those of melts from some partial melting experiments that also yield dry rhyolite melts. The hydrous mineral-free narrow mineral compositions and low-Al2O3 affinities of the IAR rhyolites are produced from basaltic middle crust under anhydrous low-temperature melting conditions. The IAR basalt lavas display prominent across-arc variation, with depleted elemental compositions in the volcanic front side and enriched compositions in the rear-arc side. The across-arc variation reflects gradual change in the slab-derived components, as demonstrated by decreasing Ba/Zr and Th/Zr values to the rear-arc side. Rhyolite lavas exhibit different across-arc variations in either the fluid-mobile elements or the immobile elements, such as Nb/Zr, La/Yb, and chondrite-normalized rare earth element patterns, reflecting that the felsic magmas had different source. The preexisting arc crust formed during an earlier stage of arc evolution, most probably during the Oligocene prior to spreading of the Shikoku back-arc basin. The lack of systematic across-arc variation in the IAR rhyolites and their dry/shallow crustal melting origin combines to suggest re-melting of preexisting Oligocene middle crust by heat from the young basaltic magmatism.",
    keywords = "Across-arc geochemical variation, Bimodal volcanism, Intra-arc rifting, Izu arc, Mantle-derived basalt, Rhyolite crustal melt",
    author = "Satoru Haraguchi and Kimura, {Jun Ichi} and Ryoko Senda and Koichiro Fujinaga and Kentaro Nakamura and Yutaro Takaya and Teruaki Ishii",
    year = "2017",
    month = "5",
    day = "1",
    doi = "10.1007/s00410-017-1345-1",
    language = "English",
    volume = "172",
    journal = "Contributions to Mineralogy and Petrology",
    issn = "0010-7999",
    publisher = "Springer Verlag",
    number = "5",

    }

    TY - JOUR

    T1 - Origin of felsic volcanism in the Izu arc intra-arc rift

    AU - Haraguchi, Satoru

    AU - Kimura, Jun Ichi

    AU - Senda, Ryoko

    AU - Fujinaga, Koichiro

    AU - Nakamura, Kentaro

    AU - Takaya, Yutaro

    AU - Ishii, Teruaki

    PY - 2017/5/1

    Y1 - 2017/5/1

    N2 - An intra-arc rift (IAR) is developed behind the volcanic front in the Izu arc, Japan. Bimodal volcanism, represented by basalt and rhyolite lavas and hydrothermal activity, is active in the IAR. The constituent minerals in the rhyolite lavas are mainly plagioclase and quartz, whereas mafic minerals are rare and are mainly orthopyroxene without any hydrous minerals such as amphibole and biotite. Both the phenocryst and groundmass minerals have felsic affinities with a narrow compositional range. The petrological and bulk chemical characteristics are similar to those of melts from some partial melting experiments that also yield dry rhyolite melts. The hydrous mineral-free narrow mineral compositions and low-Al2O3 affinities of the IAR rhyolites are produced from basaltic middle crust under anhydrous low-temperature melting conditions. The IAR basalt lavas display prominent across-arc variation, with depleted elemental compositions in the volcanic front side and enriched compositions in the rear-arc side. The across-arc variation reflects gradual change in the slab-derived components, as demonstrated by decreasing Ba/Zr and Th/Zr values to the rear-arc side. Rhyolite lavas exhibit different across-arc variations in either the fluid-mobile elements or the immobile elements, such as Nb/Zr, La/Yb, and chondrite-normalized rare earth element patterns, reflecting that the felsic magmas had different source. The preexisting arc crust formed during an earlier stage of arc evolution, most probably during the Oligocene prior to spreading of the Shikoku back-arc basin. The lack of systematic across-arc variation in the IAR rhyolites and their dry/shallow crustal melting origin combines to suggest re-melting of preexisting Oligocene middle crust by heat from the young basaltic magmatism.

    AB - An intra-arc rift (IAR) is developed behind the volcanic front in the Izu arc, Japan. Bimodal volcanism, represented by basalt and rhyolite lavas and hydrothermal activity, is active in the IAR. The constituent minerals in the rhyolite lavas are mainly plagioclase and quartz, whereas mafic minerals are rare and are mainly orthopyroxene without any hydrous minerals such as amphibole and biotite. Both the phenocryst and groundmass minerals have felsic affinities with a narrow compositional range. The petrological and bulk chemical characteristics are similar to those of melts from some partial melting experiments that also yield dry rhyolite melts. The hydrous mineral-free narrow mineral compositions and low-Al2O3 affinities of the IAR rhyolites are produced from basaltic middle crust under anhydrous low-temperature melting conditions. The IAR basalt lavas display prominent across-arc variation, with depleted elemental compositions in the volcanic front side and enriched compositions in the rear-arc side. The across-arc variation reflects gradual change in the slab-derived components, as demonstrated by decreasing Ba/Zr and Th/Zr values to the rear-arc side. Rhyolite lavas exhibit different across-arc variations in either the fluid-mobile elements or the immobile elements, such as Nb/Zr, La/Yb, and chondrite-normalized rare earth element patterns, reflecting that the felsic magmas had different source. The preexisting arc crust formed during an earlier stage of arc evolution, most probably during the Oligocene prior to spreading of the Shikoku back-arc basin. The lack of systematic across-arc variation in the IAR rhyolites and their dry/shallow crustal melting origin combines to suggest re-melting of preexisting Oligocene middle crust by heat from the young basaltic magmatism.

    KW - Across-arc geochemical variation

    KW - Bimodal volcanism

    KW - Intra-arc rifting

    KW - Izu arc

    KW - Mantle-derived basalt

    KW - Rhyolite crustal melt

    UR - http://www.scopus.com/inward/record.url?scp=85017034604&partnerID=8YFLogxK

    UR - http://www.scopus.com/inward/citedby.url?scp=85017034604&partnerID=8YFLogxK

    U2 - 10.1007/s00410-017-1345-1

    DO - 10.1007/s00410-017-1345-1

    M3 - Article

    AN - SCOPUS:85017034604

    VL - 172

    JO - Contributions to Mineralogy and Petrology

    JF - Contributions to Mineralogy and Petrology

    SN - 0010-7999

    IS - 5

    M1 - 25

    ER -