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The eruption history and silicic magma systems of caldera-forming eruptions in eastern Hokkaido; Japan

机译:北海道东部火山口形成喷发的喷发历史和硅质岩浆系统;日本

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摘要

The eruptive history and magma systems of large-scale explosive eruptions (VEI >5) in eastern Hokkaido; Japan; are reviewed on the basis of recently reported high-resolution tephrostratigraphy. More than 70 large-scale explosive eruptions have been recorded from the Akan; Kutcharo; Atosanupuri; and Mashu caldera volcanoes in the past 1.7 Ma. The total tephra volume of these eruptions is estimated to be approximately 1000 km3. The discharge rate increases remarkably from 0.2 km3/kyr to 2.0 km_3/kyr at approximately 0.2 Ma. The discharge rate is still high owing to the recent frequent activity of the Mashu caldera. The silicic magma systems of the Akan; Kutcharo; and Mashu calderas formed independently. On the other hand; the magma of Atosanupuri is associated with that of Kutcharo caldera.
机译:北海道东部大规模爆炸爆发(VEI> 5)的爆发历史和岩浆系统;日本;根据最近报道的高分辨率断层地层照相术进行了回顾。阿肯族人已记录到70多次大规模爆炸事件。 Kutcharo; Atosanupuri;和过去1.7 Ma的玛舒火山口火山。这些火山喷发的总提夫拉体积估计约为1000 km3。放电速率在大约0.2 Ma时从0.2 km3 / kyr显着增加到2.0 km_3 / kyr。由于马舒火山口最近的频繁活动,其出院率仍然很高。阿肯人的硅质岩浆系统; Kutcharo;和玛舒火山口独立形成。另一方面; Atosanupuri的岩浆与Kutcharo破火山口的岩浆有关。

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