山陰地方西部沖の神田岬沖断層周辺の海底段丘と発達過程
広島大学文学部論集 Volume 81
Page 19-38
published_at 2021-12-25
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Title ( jpn ) |
山陰地方西部沖の神田岬沖断層周辺の海底段丘と発達過程
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Title ( eng ) |
Development of Submarine Geomorphology Based on Analysis of Submarine Terraces around the Kandamisaki-oki Fault off the Coast of San-in Region
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Creator | |
Source Title |
広島大学文学部論集
The Hiroshima University studies, School of Letters
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Volume | 81 |
Start Page | 19 |
End Page | 38 |
Journal Identifire |
[PISSN] 2436-410X
[NCID] AA12917288
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Abstract |
This study aims to describe the submarine geomorphology near the Kandamisaki-oki fault off the coast of the Sanin region and examine its development. The NW-SE trending Kandamisaki-oki fault is a series of fault scarps on the seafloor and is a northwestern extension of the onshore Kikukawa fault, an active sinistral strike-slip fault. Although the distribution and activity of the Kandamisaki-oki fault have been studied, the submarine geomorphology near the fault has been ignored.
This study produced a topographical anaglyph image using a 0.3-s-mesh digital elevation model that used point-cloud data obtained through a multi-beam acoustic survey by the Japan Coast Guard. The image was exaggerated vertically and overlapped with a relief map and an isobath. When viewed with red-cyan glasses, it enables easy identification of topographical features, such as submarine terraces and small fault scarps. By interpreting the anaglyph, the submarine terraces were divided into six surfaces, named the S1, S2, S3, S4, S5, and S6 surfaces, in descending order. The angles indicating the paleo-shoreline behind the flat surface of each submarine terrace were at a depth of approximately 30m for S1, approximately 50m for S2, approximately 80m for S3, approximately 110m for S4, approximately 120m for S5, and approximately 130m for S6. In the study area, these depths were similar and correlated to the terrace surfaces around the Tsushima Strait and the Nanseishoto islands. Therefore, the submarine terraces in the study area developed in association with the global sea-level changes resulting from the changes in the volume of the glaciers since the last glacial period. |
Keywords |
海底段丘
海底活断層
数値標高モデル
アナグリフ
菊川断層
submarine terrace
active submarine fault
digital elevation model
topographic anaglyph
Kikukawa fault
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Descriptions |
科学研究費補助金(課題番号:19H01374)の一部を使用した。
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Language |
jpn
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Resource Type | departmental bulletin paper |
Publisher |
広島大学文学部
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Date of Issued | 2021-12-25 |
Publish Type | Version of Record |
Access Rights | open access |
Source Identifier |
[ISSN] 2436-410X
[NCID] AA12917288
|