[S-TT37] 空中からの地球計測とモニタリング

[STT37-P03] 無人ヘリコプターを用いた伊豆大島高解像空中磁気測量の再解析

*小山 崇夫¹、金子 隆之¹、大湊 隆雄¹、安田 敦¹、小河 勉¹、渡邉 篤志¹、坂下 至功¹、武尾 実¹、柳澤 孝寿²、本多 嘉明³、梶原 康司³ (1.東京大学地震研究所、2.国立研究開発法人海洋研究開発機構、3.千葉大学環境リモートセンシング研究センター)

キーワード：伊豆大島、無人ヘリコプター、空中磁気測量

We conducted a high-resolution aeromagnetic survey using an autonomously driven unpersoned helicopter that flew as low as several tens of meters above the ground along precise flight tracks with 1 m accuracy. The geomagnetic total intensity was measured by a total intensity magnetometer suspended beneath the helicopter at a ~50 m or less flight spacing over the entire caldera of Mt. Mihara, located on Izu-Oshima Island, Japan. From the observed geomagnetic data, we estimated high-resolution subsurface magnetization intensity. A high average magnetization intensity of 13.5 A/m was obtained for the entire caldera. The distribution of the magnetization intensity was not only consistent with the results of conventional airborne surveys, but also had a high spatial resolution of less than 100 m. Highly magnetized areas were observed along the NW–SE lines that intersected the summit pit crater, the Crater A, which is consistent with the principal stress direction of Izu-Oshima Island. These highly magnetized areas might be solidified magma that did not reach the surface during past eruptions. A large and deep-rooted weakly magnetized area was found just outside of the NE side of the central cone. It corresponds to the location of the Fissure B, and the conduit must be demagnetized at the previous event. Other weakly magnetized areas were also observed at the North, East and SW sides around the pit crater. These regions corresponds to the location of fumaroles in the crater. The high-resolution subsurface magnetization imaged by the autonomous unpersoned helicopter is helpful for mitigating future eruption damage by enabling the assessment of potential fissure eruption areas.