日本地球惑星科学連合2025年大会

講演情報

[J] ポスター発表

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-CG54] 岩石―流体相互作用の新展開:表層から沈み込み帯深部まで

2025年5月30日(金) 17:15 〜 19:15 ポスター会場 (幕張メッセ国際展示場 7・8ホール)

コンビーナ:岡本 敦(東北大学大学院環境科学研究科)、武藤 潤(東北大学大学院理学研究科地学専攻)、片山 郁夫(広島大学大学院先進理工系科学研究科地球惑星システム学プログラム)、中島 淳一(東京科学大学理学院地球惑星科学系)

17:15 〜 19:15

[SCG54-P03] 深層学習による岩石CT画像の深さ方向超解像

*香川 龍吾1岡本 敦2大森 敏明1 (1.神戸大学、2.東北大学)

キーワード:超解像、深層学習、データ駆動アプローチ、岩石CT画像

In recent years, rock CT images obtained from geological studies have been paid much attention in earth and environment science to understand geomaterials and underground resources in earth. However, rock CT images have a low-resolution in depth direction due to time and environmental constraint while three-dimensional structure is important to understand geological properties. In order to reveal earth geological structure, it is important to establish a super-resolution method for rock CT images in the depth direction.
In this study, we propose a super-resolution method for estimating three-dimensional rock CT images by deep learning. Rock CT images used in this study are obtained from Oman drilling project and consist of serpentinite, hydrolite, magnetite, and Cr-rich spinel. We construct our super-resolution method by applying frame interpolation concepts based on temporal image flows reflecting dynamical properties of image data. In the proposed method, we estimate an unobservable rock CT image by spatially neighboring CT images by depth directional interpolation. We apply optical flows between observable multiple input CT images to generate an intermediate CT image at unobservable depth. We show the effectiveness of the proposed method by comparing intermediate CT image estimated by our proposed method with intermediate one estimated by conventional method qualitatively and quantitatively.