日本地球惑星科学連合2025年大会

講演情報

[J] 口頭発表

セッション記号 S (固体地球科学) » S-CG 固体地球科学複合領域・一般

[S-CG55] 海洋底地球科学

2025年5月27日(火) 13:45 〜 15:15 コンベンションホール (CH-A) (幕張メッセ国際会議場)

コンビーナ:飯沼 卓史(国立研究開発法人 海洋研究開発機構)、藤井 昌和(国立極地研究所 / 総合研究大学院大学)、尾張 聡子(東京海洋大学)、山本 揚二朗(海洋研究開発機構)、座長:安川 和孝(東京大学大学院工学系研究科エネルギー・資源フロンティアセンター)、見邨 和英(産業技術総合研究所・地質調査総合センター)


15:00 〜 15:15

[SCG55-06] 深層学習を活用した東青ヶ島カルデラにおける海底熱水活動の探査

*見邨 和英1金子 純二2野崎 達生3,4笠谷 貴史2、杉本 洋平5、玄田 貴之4中村 謙太郎4,6 (1.産総研・地質調査総合センター、2.海洋研究開発機構、3.早稲田大学、4.東京大学、5.日本海洋事業、6.千葉工業大学)

キーワード:海底鉱物資源、海底熱水鉱床、深層学習、物体検出

Seafloor massive sulfide deposits are expected to be a prominent resource for various metals such as Pb, Zn, Pb, Au, Ag [1, 2]. Previous studies have shown that the signatures of hydrothermal activities can be detected as acoustic scattering anomalies in the water column images obtained by multi-beam echo sounder (MBES images) [3–5]. However, the conventional method required skilled observers carefully observing numerous MBES images to detect hydrothermal emission signals, which have required enormous time and efforts.
Recently, we have shown that object detection, a type of deep learning (DL) technique, is applicable to finding the signals from MBES images, which is fast enough for real-time observations [6]. We have also proposed a method to reduce false positives (misdetections) by time-series analysis [7].
Here, we report the practical application of the DL-based observations. MBES images were captured during research cruises KM22-11C, KM23-01 and KM23-02 at the Higashi-Aogashima Knoll Caldera hydrothermal site, Izu-Bonin Arc. First, we have confirmed the applicability of the DL system by surveying on known sites. Then, a wide-area survey within the caldera was conducted. The DL model successfully identified prominent sites of hydrothermal activities based on a vast number of images. Notably, during the succeeding cruises KM23-08_09C and KM24-09, an existence of the hydrothermal activity was newly confirmed from one of the prominent sites by ROV survey.

References:
[1] Hannington et al. (2011) Geology, 39, 1155–1158.; [2] Iizasa et al. (2019) Mineralium Deposita, 54, 117–132.; [3] Nakamura et al. (2015) Geochem. J., 49, 579–596.; [4] Kasaya et al. (2015) Geochem. J., 49, 597–602.; [5] Kaneko and Kasaya (2022) Geoinformatics, 33, 87–94. [6] Mimura et al. (2023) IEEE-JSTARS, 16, 2703–2710.; [7] Genda et al. (2025) TechRxiv. https://doi.org/10.36227/techrxiv.173895078.87591845/v1.