{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1390584342829138560.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.9795/bullgsj.75.5-6_197"}},{"identifier":{"@type":"URI","@value":"https://www.jstage.jst.go.jp/article/bullgsj/75/5-6/75_197/_pdf"}}],"dc:title":[{"@language":"en","@value":"Shallow submarine structure around Tokara Islands based on the high-resolution subbottom profiler survey during the GS22 cruise"},{"@language":"ja","@value":"GS22 航海での高分解能サブボトムプロファイラー探査に基づく トカラ列島周辺海域の海底下浅部構造"}],"dc:language":"ja","description":[{"type":"abstract","notation":[{"@language":"en","@value":"<p>During the GS22 cruise of the <i>R/V Shinyo Maru</i> (The Tokyo University of Marine Science and Technology) from May to June 2022, a high-resolution subbottom profiler (SBP) survey was conducted, focusing on the area of the Tokara Islands and Yakushima Island to obtain geological information on the shallow subbottom structure in the area. This paper summarizes the shallow subbottom structure around Yakushima and Takarajima Islands, as revealed by the SBP surveys. Although the internal structure of the sedimentary sequences could not be determined over most of the continental shelf in the area north of Yakushima Island, we identified partially stratified sedimentary sequences with a maximum thickness of ~20 m below the seafloor. The SBP profiles revealed the internal structure of stratified sedimentary sequences down to a maximum of 40 m below the seafloor in the volcanic front area located west of Yakushima Island. The partially stratified sedimentary sequences occur between the volcanic front area and the western slope of the Tane-Yaku Spur, a characteristic bathymetric high between Yakushima and Tanegashima Islands, although most of the internal structure could not be identified due to poor penetration of acoustic waves. We also surveyed the area north of Takarajima Island, where many earthquakes have occurred in recent years, suggesting the presence of seafloor movement related to seismic activity. However, the data indicate that no faults or intrusion structures have reached the seafloor or shallow part of the sedimentary sequences in this region.</p>"},{"@language":"ja","@value":"<p>GS22航海では，2022年5月から6月の期間に東京海洋大学の神鷹丸を用いて，トカラ列島周辺海域で高分解能サブボトムプロファイラー探査を行い，本海域の海底下浅部に関する地質情報を取得した．本論では，屋久島周辺海域及び宝島北方海域でのSBP探査により明らかになった海底下浅部の地質構造をまとめる．屋久島の周辺部のうち，屋久島北方沖では陸棚部分の堆積層の内部構造は不明であったが，部分的に成層した層厚が海底面下最大20 m程度の堆積層が認められた．屋久島西方沖の火山フロント域では海底面下最大約40 mまで成層した堆積層の内部構造を把握できた．屋久島南方沖の火山フロント域及び種子–屋久海脚の部分では，部分的に成層した堆積層が認められるが，音波の透過が悪く内部構造の大部分は不鮮明であった．また，近年地震が群発している宝島北方沖の観測では地震活動に関連した海底変動の存在を想定したが，海底に到達した断層及び下部からの貫入構造などは認められなかった．</p>"}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410584342829138564","@type":"Researcher","foaf:name":[{"@language":"en","@value":"MISAWA Ayanori"},{"@language":"ja","@value":"三澤 文慶"}],"jpcoar:affiliationName":[{"@language":"en","@value":"AIST, Geological Survey of Japan, Research Institute of Geology and Geoinformation"},{"@language":"ja","@value":"産業技術総合研究所 地質調査総合センター地質情報研究部門"}]},{"@id":"https://cir.nii.ac.jp/crid/1410584342829138565","@type":"Researcher","foaf:name":[{"@language":"en","@value":"FURUYAMA Seishiro"},{"@language":"ja","@value":"古山 精史朗"}],"jpcoar:affiliationName":[{"@language":"ja","@value":"国立大学法人東京海洋大学海洋資源環境学部"},{"@language":"en","@value":"Tokyo University of Marine Science and Technology, School of Marine Resources and Environment"}]},{"@id":"https://cir.nii.ac.jp/crid/1410584342829138563","@type":"Researcher","foaf:name":[{"@language":"en","@value":"KOGE Hiroaki"},{"@language":"ja","@value":"高下 裕章"}],"jpcoar:affiliationName":[{"@language":"ja","@value":"産業技術総合研究所 地質調査総合センター地質情報研究部門"},{"@language":"en","@value":"AIST, Geological Survey of Japan, Research Institute of Geology and Geoinformation"}]},{"@id":"https://cir.nii.ac.jp/crid/1410584342829138560","@type":"Researcher","foaf:name":[{"@language":"en","@value":"ARIMOTO Jun"},{"@language":"ja","@value":"有元 純"}],"jpcoar:affiliationName":[{"@language":"ja","@value":"産業技術総合研究所 地質調査総合センター地質情報研究部門"},{"@language":"en","@value":"AIST, Geological Survey of Japan, Research Institute of Geology and Geoinformation"}]},{"@id":"https://cir.nii.ac.jp/crid/1410584342829138561","@type":"Researcher","foaf:name":[{"@language":"en","@value":"ISHINO Saki"},{"@language":"ja","@value":"石野 沙季"}],"jpcoar:affiliationName":[{"@language":"en","@value":"AIST, Geological Survey of Japan, Research Institute of Geology and Geoinformation"},{"@language":"ja","@value":"産業技術総合研究所 地質調査総合センター地質情報研究部門"}]},{"@id":"https://cir.nii.ac.jp/crid/1410584342829138562","@type":"Researcher","foaf:name":[{"@language":"en","@value":"SUZUKI Yoshiaki"},{"@language":"ja","@value":"鈴木 克明"}],"jpcoar:affiliationName":[{"@language":"ja","@value":"産業技術総合研究所 地質調査総合センター地質情報研究部門"},{"@language":"en","@value":"AIST, Geological Survey of Japan, Research Institute of Geology and Geoinformation"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"13464272"},{"@type":"LISSN","@value":"13464272"},{"@type":"EISSN","@value":"2186490X"}],"prism:publicationName":[{"@language":"en","@value":"BULLETIN OF THE GEOLOGICAL SURVEY OF JAPAN"},{"@value":"地質調査研究報告"},{"@language":"en","@value":"Bull. Geol. Surv. Japan"},{"@value":"地調研報"}],"dc:publisher":[{"@language":"en","@value":"National Institute of Advanced Industrial Science and Technology, Geological Survey of Japan"},{"@language":"ja","@value":"国立研究開発法人 産業技術総合研究所 地質調査総合センター"}],"prism:publicationDate":"2024-12-27","prism:volume":"75","prism:number":"5-6","prism:startingPage":"197","prism:endingPage":"208"},"reviewed":"false","url":[{"@id":"https://www.jstage.jst.go.jp/article/bullgsj/75/5-6/75_197/_pdf"}],"availableAt":"2024-12-27","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Tokara%20Islands","dc:title":"Tokara Islands"},{"@id":"https://cir.nii.ac.jp/all?q=Ryukyu%20Arc","dc:title":"Ryukyu Arc"},{"@id":"https://cir.nii.ac.jp/all?q=Volcanic%20front","dc:title":"Volcanic front"},{"@id":"https://cir.nii.ac.jp/all?q=Okinawa%20Trough","dc:title":"Okinawa Trough"},{"@id":"https://cir.nii.ac.jp/all?q=Subbottom%20Profiler%20(SBP)","dc:title":"Subbottom Profiler (SBP)"},{"@id":"https://cir.nii.ac.jp/all?q=Submarine%20shallow%20structure","dc:title":"Submarine shallow structure"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360013267311712000","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Volcanic and tectonic features of Shirahama Bank in the northern Ryukyu Arc: Implications for cross-arc volcanism controlled by arc-parallel extension"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567866336512","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A model for the motion of the Philippine Sea Plate consistent with NUVEL‐1 and geological data"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318730008704","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Detailed morphology and bubble plumes of Daiichi-Amami Knoll in the central Ryukyu Arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204230745088","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Mid-Pleistocene Submarine Acidic Volcanism of the Tokara Islands, Japan"},{"@language":"ja","@value":"トカラ列島における中期更新世の酸性海底火山活動"},{"@language":"ja-Kana","@value":"トカラ レットウ ニ オケル チュウキ コウシン セイ ノ サンセイ カイテイ カザン カツドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205448104320","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"「情報地質研究会」の発足と「情報地質」の刊行継続について"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206238521984","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geotectonic Framework of the Ryukyu Islands (Nansei-shoto)"},{"@value":"琉球列島(南西諸島)の構造区分"},{"@language":"ja-Kana","@value":"リュウキュウ レットウ ナンセイ ショトウ ノ コウゾウ クブン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390017289897048704","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"GS21 航海での高分解能サブボトムプロファイラー探査に基づく トカラ列島周辺海域の海底下浅部構造"},{"@language":"en","@value":"Shallow submarine structure around Tokara Islands based on the high-resolution subbottom profiler survey during the GS21 cruise"},{"@language":"ja-Kana","@value":"GS21 コウカイ デ ノ コウブンカイノウ サブボトムプロファイラー タンサ ニ モトズク トカラ レットウ シュウヘン カイイキ ノ カイテイ カセンブ コウゾウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679207020288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Studies of Land Bridges and the Migration of Men and Other Animals along Them. Detailed Bathymetric Features of Tokara and Kerama Gaps in the Ryukyu Arc."},{"@value":"陸橋とヒトと生物の渡来　琉球弧のトカラギャップおよびケラマギャップ"},{"@language":"ja-Kana","@value":"リュウキュウコ ノ トカラ ギャップ オヨビ ケラマ ギャップ ニ オケル セ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681211856256","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Sedimentation in the Oki Trough, southern Japan Sea, as revealed by high resolution seismic records (3.5kHz echograms)."},{"@value":"高分解能音波探査記録からみた隠岐トラフの堆積作用"},{"@language":"ja-Kana","@value":"コウ ブンカイノウ オンパ タンサ キロク カラ ミタ オキ トラフ ノ タイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390294719105074304","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"GB21-1 及びGK20 航海（トカラ列島周辺海域）における海底地形観測"},{"@language":"en","@value":"The bathymetry survey around Tokara Islands during GB21-1 and GK20 cruise"},{"@language":"ja-Kana","@value":"GB21-1 オヨビ GK20 コウカイ(トカラ レットウ シュウヘン カイイキ)ニ オケル カイテイ チケイ カンソク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390294719105100416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"GK20 航海での高分解能サブボトムプロファイラー探査に基づく トカラ列島周辺海域の海底下浅部構造"},{"@language":"en","@value":"Shallow submarine structure around Tokara Islands based on the high-resolution subbottom profiler survey during the GK20 cruise"},{"@language":"ja-Kana","@value":"GK20 コウカイ デ ノ コウブンカイノウ サブボトムプロファイラー タンサ ニ モトズク トカラ レットウ シュウヘン カイイキ ノ カイテイ カセンブ コウゾウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390298764873760128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"GB21-2，3 トカラ列島周辺海域におけるマルチビーム測深器による観測の概要"},{"@language":"en","@value":"Results of the multibeam echo sounder observations on the GB21-2,3 cruises (around Tokara Islands)"},{"@language":"ja-Kana","@value":"GB21-2,3 トカラ レットウ シュウヘン カイイキ ニ オケル マルチビーム ソクシンキ ニ ヨル カンソク ノ ガイヨウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390584342829136384","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Special issue on marine geology around Tokara Islands in Kagoshima prefecture: result of marine geological mapping survey cruses in 2022 Fiscal Year"},{"@language":"ja","@value":"鹿児島県トカラ列島周辺の海洋地質−2022年度調査航海結果−"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317012916224","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seismic evidence for arc segmentation, active magmatic intrusions and syn-rift fault system in the northern Ryukyu volcanic arc"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714791996725632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seismic structure of rifting in the Okinawa Trough, an active backarc basin of the Ryukyu (Nansei-Shoto) island arc–trench system"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:2013679458"},{"@type":"CROSSREF","@value":"10.9795/bullgsj.75.5-6_197"},{"@type":"CROSSREF","@value":"10.9795/bullgsj.75.5-6_161_references_DOI_DjjzI1H62GfjTXgGEaR3kO7Umyk"}]}