Miocene submarine fire fountain deposits, ryugazaki headland, oshoro peninsula, hokkaido, japan: Implications for submarine fountain dynamics and fragmentation processes

Raymond Alexander Fernand Cas, H Yamagishi, L Moore, Ceinwen Scutter

    Research output: Chapter in Book/Report/Conference proceedingChapter (Book)Researchpeer-review

    Abstract

    Three in situ Miocene submarine basaltic andesite fire fountain deposits are preserved at Ryugazaki Headland, Oshoro Peninsula, Hokkaido, Japan. Emplacement occurred below storm wave base based on the absence of shallow water fractional reworking structures. The basal facies is a mass flow resedimented pillow clast and spatter clast breccia, indicating early effusive pillow lava and fire fountain eruptive activity upslope from the depositional site. The overlying fire fountain deposits consist of a porphyritic spatter clast breccia facies [oldest], an aphyric spatter micro-breccia facies, and a spheroidal clast breccia facies [youngest]. Only the youngest has a feeder dike exposed. The aphyric spatter micro-breccia facies indicates a high submarine fountain, fed by a high magma discharge, low viscosity magma source. Abundant blocky matrix clasts, indicate pervasive quench fragmentation in the high fire fountain. The fountains for the porphyritic spatter breccia and spheroidal clast breccia were lower, less water was able to enter the fountain, producing less quench fragmentation, and coarser deposits. In submarine fire fountains, the primary fragmentation process is shearing and extensional stretching of the magma fountain as it flares above the vent and decelerates. Quench fragmentation is an important second-order fragmentation process, especially at the margins of the fountain. The low vesicularity of Ryugazaki spatter [generally < 30%] indicates that explosive magmatic vesiculation was not an important process, and there is no direct evidence for phreatomagmatic influences. Spatter debris was deposited by fallout, with only minor evidence for re-sedimentation.

    Original languageEnglish
    Title of host publicationExplosive Subaqueous Volcanism
    EditorsJ D L White, J L Smellie, D A Clague
    Place of PublicationWashington USA
    PublisherAmerican Geophysical Union
    Pages299-316
    Number of pages18
    ISBN (Electronic)9781118668665
    ISBN (Print)9780875909998
    DOIs
    Publication statusPublished - 1 Jan 2003

    Publication series

    NameGeophysical Monograph Series
    Volume140
    ISSN (Print)0065-8448
    ISSN (Electronic)2328-8779

    Cite this

    Cas, R. A. F., Yamagishi, H., Moore, L., & Scutter, C. (2003). Miocene submarine fire fountain deposits, ryugazaki headland, oshoro peninsula, hokkaido, japan: Implications for submarine fountain dynamics and fragmentation processes. In J. D. L. White, J. L. Smellie, & D. A. Clague (Eds.), Explosive Subaqueous Volcanism (pp. 299-316). (Geophysical Monograph Series; Vol. 140). Washington USA: American Geophysical Union. https://doi.org/10.1029/140GM20
    Cas, Raymond Alexander Fernand ; Yamagishi, H ; Moore, L ; Scutter, Ceinwen. / Miocene submarine fire fountain deposits, ryugazaki headland, oshoro peninsula, hokkaido, japan : Implications for submarine fountain dynamics and fragmentation processes. Explosive Subaqueous Volcanism. editor / J D L White ; J L Smellie ; D A Clague. Washington USA : American Geophysical Union, 2003. pp. 299-316 (Geophysical Monograph Series).
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    title = "Miocene submarine fire fountain deposits, ryugazaki headland, oshoro peninsula, hokkaido, japan: Implications for submarine fountain dynamics and fragmentation processes",
    abstract = "Three in situ Miocene submarine basaltic andesite fire fountain deposits are preserved at Ryugazaki Headland, Oshoro Peninsula, Hokkaido, Japan. Emplacement occurred below storm wave base based on the absence of shallow water fractional reworking structures. The basal facies is a mass flow resedimented pillow clast and spatter clast breccia, indicating early effusive pillow lava and fire fountain eruptive activity upslope from the depositional site. The overlying fire fountain deposits consist of a porphyritic spatter clast breccia facies [oldest], an aphyric spatter micro-breccia facies, and a spheroidal clast breccia facies [youngest]. Only the youngest has a feeder dike exposed. The aphyric spatter micro-breccia facies indicates a high submarine fountain, fed by a high magma discharge, low viscosity magma source. Abundant blocky matrix clasts, indicate pervasive quench fragmentation in the high fire fountain. The fountains for the porphyritic spatter breccia and spheroidal clast breccia were lower, less water was able to enter the fountain, producing less quench fragmentation, and coarser deposits. In submarine fire fountains, the primary fragmentation process is shearing and extensional stretching of the magma fountain as it flares above the vent and decelerates. Quench fragmentation is an important second-order fragmentation process, especially at the margins of the fountain. The low vesicularity of Ryugazaki spatter [generally < 30{\%}] indicates that explosive magmatic vesiculation was not an important process, and there is no direct evidence for phreatomagmatic influences. Spatter debris was deposited by fallout, with only minor evidence for re-sedimentation.",
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    Cas, RAF, Yamagishi, H, Moore, L & Scutter, C 2003, Miocene submarine fire fountain deposits, ryugazaki headland, oshoro peninsula, hokkaido, japan: Implications for submarine fountain dynamics and fragmentation processes. in JDL White, JL Smellie & DA Clague (eds), Explosive Subaqueous Volcanism. Geophysical Monograph Series, vol. 140, American Geophysical Union, Washington USA, pp. 299-316. https://doi.org/10.1029/140GM20

    Miocene submarine fire fountain deposits, ryugazaki headland, oshoro peninsula, hokkaido, japan : Implications for submarine fountain dynamics and fragmentation processes. / Cas, Raymond Alexander Fernand; Yamagishi, H; Moore, L; Scutter, Ceinwen.

    Explosive Subaqueous Volcanism. ed. / J D L White; J L Smellie; D A Clague. Washington USA : American Geophysical Union, 2003. p. 299-316 (Geophysical Monograph Series; Vol. 140).

    Research output: Chapter in Book/Report/Conference proceedingChapter (Book)Researchpeer-review

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    Cas RAF, Yamagishi H, Moore L, Scutter C. Miocene submarine fire fountain deposits, ryugazaki headland, oshoro peninsula, hokkaido, japan: Implications for submarine fountain dynamics and fragmentation processes. In White JDL, Smellie JL, Clague DA, editors, Explosive Subaqueous Volcanism. Washington USA: American Geophysical Union. 2003. p. 299-316. (Geophysical Monograph Series). https://doi.org/10.1029/140GM20