Identification of Zenikame-Menagawa Tephra Using Major Element Compositions of Amphibole Phenocrysts
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- WATANABE Hazuki
- Faculty of Science and Technology, Hirosaki University
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- OKADA Rina
- Graduate School of Science and Technology, Hirosaki University
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- UMEDA Koji
- Graduate School of Science and Technology, Hirosaki University
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- NISHIDA Yuuki
- Electric Power Development Co., Ltd.
Bibliographic Information
- Other Title
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- 角閃石族の化学組成に基づく銭亀―女那川テフラの対比
- カクセンセキゾク ノ カガク ソセイ ニ モトズク ゼニガメ-ジョナガワ テフラ ノ タイヒ
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Abstract
<p>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.</p>
Journal
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- Journal of the Japan Society of Engineering Geology
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Journal of the Japan Society of Engineering Geology 63 (5), 228-236, 2022-12-10
Japan Society of Engineering Geology
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Details 詳細情報について
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- CRID
- 1390295104416683264
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- NII Book ID
- AN00026635
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- ISSN
- 18840973
- 02867737
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- NDL BIB ID
- 032590128
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- Text Lang
- ja
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- Data Source
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- JaLC
- NDL
- Crossref
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- Abstract License Flag
- Disallowed