Journal of the Japan Society of Engineering Geology
Online ISSN : 1884-0973
Print ISSN : 0286-7737
ISSN-L : 0286-7737
Volume 63, Issue 5
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  • Hazuki WATANABE, Rina OKADA, Koji UMEDA, Yuuki NISHIDA
    2022 Volume 63 Issue 5 Pages 228-236
    Published: December 10, 2022
    Released on J-STAGE: February 14, 2023
    JOURNAL FREE ACCESS

    Petrochemistry of the mafic minerals played an important role in the identification and correlation of tephra layers that include few glass shards, due to chemical weathering and/or alteration. The analyses are applied to the correlation of the Zenikame-Menagawa tephra(Z-M)in the Tokachi district, eastern Hokkaido, with those erupted from Zenikame volcano, located about 200 km west of the district. By utilizing quantitative major element analysis of amphiboles, distal Z-M tephra layers are recognized to be interbedded with the eruptive deposits, derived from Kuttara volcano. Accordingly, the eruption age of the Z-M is estimated to be between 44.1 and ca. 54 ka.

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Serialization Course Key Points of Civil Engineering Geological Investigation in Geological Bodies
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