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- 荒牧 重雄
- 東京大学地震研究所
書誌事項
- タイトル別名
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- Notes on the Geology of Kuchi-no-erabu Volcano, Southern Japan
- クチエラブジマ チシツ チョウサ ホウコク
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抄録
Kuchi-no-erabu volcano, about 70 km south of Kyushu, Japan, consists of dissected aggregates of older volcanic bodies covered by several younger cones. Most of the rocks are hypersthene-augite andesite. Shin-dake, the youngest cone, has been frequently active, displaying a Vulcanian-type eruptions at the summit crater. The cone is made up of stratified pyroclastic material with a few thick lava flows reaching the sea coast. The 1966 eruption of Shin-dake produced only accessory blocks, lapilli, and ash and no essential material was found. Very small-scale, low-temperature pyroclastic flow was produced at the time of the eruption. A deposit of welded pyroclastic materials on the western coast as described by MATUMOTO (1934) appears to be a product of local pyroclastic eruption.
収録刊行物
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- 火山.第2集
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火山.第2集 14 (3), 127-132, 1969
特定非営利活動法人 日本火山学会
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詳細情報 詳細情報について
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- CRID
- 1390001206121508608
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- NII論文ID
- 110002988358
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- NII書誌ID
- AN10512786
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- ISSN
- 04534360
- 24330590
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- NDL書誌ID
- 8144324
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- 本文言語コード
- ja
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- データソース種別
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- JaLC
- NDL
- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可