著者

大島 治

出版者

一般社団法人 日本地質学会

雑誌

日本地質学会学術大会講演要旨 第106年学術大会(99’名古屋) (ISSN:13483935)

巻号頁・発行日

pp.99, 1999-10-05 (Released:2017-08-24)

著者

早川 由紀夫 荒牧 重雄 白尾 元理 小林 哲夫 徳田 安伸 津久井 雅志 加藤 隆 高田 亮 小屋口 剛博 小山 真人 藤井 敏嗣 大島 治 曽屋 龍典 宇都 浩三

出版者

特定非営利活動法人日本火山学会

雑誌

火山. 第2集 (ISSN:04534360)

巻号頁・発行日

vol.29, pp.S208-S220, 1984-12-28

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Stratigraphy and thickness distribution of the pyroclastic fall deposits formed during the eruption of Miyakejima volcano on October 3-4, 1983, were studied immediately after the deposition. Of the total mass of 20 million tons erupted, 8.5 million tons were ejected as basaltic scoria to form a complex set of air-fall deposits east of the fissure vents. One million tons of the latter were ejected from the upper fissures as fire-fountain products. The rest was the product of phreatomagmatic explosions which occurred in the lower fissures where ground water chilled the magma to form dense scoria blocks which devastated villages. Explosion craters and a tuff ring were formed along the N-S trending lower fissures. Account of the general distribution of the deposits, nature of the constituents, mutual stratigraphic correlation and correlation with observed sequence are given.

著者

高田 亮 大島 治 荒牧 重雄 小野 晃司 吉田 克史 梶間 和彦

出版者

The Volcanological Society of Japan

雑誌

火山 (ISSN:04534360)

巻号頁・発行日

vol.37, no.5, pp.233-250, 1992-11-15 (Released:2017-03-20)

参考文献数

34

被引用文献数

1

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The subaerial history of Aogashima volcano (about 3 km3 in volume) was studied. The sequence of volcanic activity is summarized as follows: the growth of Kurosaki volcano (0.3 km3 in volume; basalt>andesite) in the northwestern area of Aogashima island; the construction of the main edifice of Main stratocone (basalt≫andesite) in the southeastern area; the fissure eruptions of Aphyric basalts (<0.1km3 in volume) on the northwestern flank; a surge activity (Ojiroike surge deposits) (basalt>ndesite) at about 3,000 y.B.P.; the eruptions of Kintagaura lavas (0.15 km3 in volume) filing the Southeasern basin, and airfalls (Yasundogo airfalls tephras) (0.4 km3 in volume; basalt>andesite) on the east and north flanks 3,000-2,400 y.B.P.; the occurrence of a debris avalanche (Nagashizaka debris avalanche deposits) associated with the formation of the Ikenosawa crater (1.7 km×1.5 km insize); the Tenmei (A.D. 1781-1785) eruption (0.08km3 in volume; andesite). Based on the historical records and the geological data obtained in this study, the sequence of the Tenmei eruption is restored as follows: according to historical records, a small ash eruption occurred in 1781; in 1783, the Tenmei eruption began with an explosive scoria effusion (Tenmei airfall tephras 1) associated with cone building (Maruyama pyroclastic cone); in 1785, ash fall continued intermittently for more than one month (Tenmei airfall tephras 2); finally, the Ikenosawa crater was filled with lava flows (Tenmei lavas 1 and 2). During the development of Aogashima volcano, magma paths were shifted over a distance of about 4 km. Some geological units derived from different magma paths have different, parallel trends of chemical composition in SiO2 vs. oxide diagrams. The chemical composition of magma changed with the shift in magma path. Each trend consists of a combination of plagioclase accumulation and crystallization. The magma-supply rate of Aogashima volcano was fluctuating in time and space with the growth of each geological unit, which may have led to the generation of andesite magma.

著者

大島 治子 加藤 雪彦 古賀 道之 池田 良一

雑誌

東京医科大学雑誌 (ISSN:00408905)

巻号頁・発行日

vol.60, no.1, pp.59-64, 2002-04-15

著者

宇井 忠英 隅田 まり 大学合同観測班地質班 荒牧 重雄 大島 治 鎌田 桂子 小林 武彦 小屋口 剛博 佐藤 博明 中川 光弘 中田 節也 藤井 敏嗣 藤縄 明彦 古山 勝彦 三宅 康幸 横瀬 久芳 渡辺 一徳

出版者

特定非営利活動法人日本火山学会

雑誌

火山 (ISSN:04534360)

巻号頁・発行日

vol.38, no.2, pp.45-52, 1993-07-01

被引用文献数

2

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Small-scale pyroclastic flows due to the collapse of the lava dome have been frequently generated during the 1991-93 eruption of Unzen Volcano. We have recorded video footages which show the generation of pyroclastic flows during January-March 1992. Two types of phenomena have been observed : deformation of the lava dome due to flowage ; and a sudden discharge of gas and ash through fractures and peeling-off of rock fragments from the surface of cooling lava blocks. Pyroclastic flows were generated only in places on the lava dome where these precursory phenomena were frequently observed.