JpGU-AGU Joint Meeting 2017

講演情報

[EJ] 口頭発表

セッション記号 S (固体地球科学) » S-GL 地質学

[S-GL34] [EJ] 「泥火山」の新しい研究展開に向けて

2017年5月20日(土) 15:30 〜 17:00 A04 (東京ベイ幕張ホール)

コンビーナ:浅田 美穂(国立研究法人海洋研究開発機構)、土岐 知弘(琉球大学理学部)、井尻 暁(国立研究開発法人海洋研究開発機構)、辻 健(九州大学カーボンニュートラル・エネルギー国際研究所)、座長:土岐 知弘(琉球大学理学部)、座長:辻 健(九州大学カーボンニュートラル・エネルギー国際研究所)

16:43 〜 16:58

[SGL34-05] 北部琉球弧喜界島周辺海域に分布する泥火山

*板木 拓也1佐藤 太一1井上 卓彦1天野 敦子1田中 裕一郎1 (1.産業技術総合研究所)

Geological Survey of Japan have carried out research cruises around the Ryukyu Arc since 2008 in order to improve geoinformation of Japan. During three cruises GH14, GK14 and GK15-2 in 2014 and 2015, we found at least eleven mud volcanoes around the Kikai-jima Island of northern Ryukyu Arc using multi-narrow beam survey system. The largest mud volcano with 1-km diameter of the caldera is located at 17 km off SSW of the Kikai-jima Island (water depth: 400 m). Surface deposition collected by a grab sampler from the caldera is composed of grayish silty clay including many subangular pebbles. These pebbles were likely carried from old strata below the sea-floor when the mud volcano erupted in relatively near the past. To investigate erupted ages of the mud volcano may be important for understanding their relation to the fault activity at the forearc region.