{"@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/1361981470161183360.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1023/a:1004818225642"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/content/pdf/10.1023/A:1004818225642.pdf"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/article/10.1023/A:1004818225642/fulltext.html"}},{"identifier":{"@type":"NAID","@value":"30012562677"}}],"dc:title":[{"@value":"Giant Megamullion in the Parece Vela Backarc Basin"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381981470161183361","@type":"Researcher","foaf:name":[{"@value":"Yasuhiko Ohara"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981470161183363","@type":"Researcher","foaf:name":[{"@value":"Tsuyoshi Yoshida"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981470161183362","@type":"Researcher","foaf:name":[{"@value":"Yukihiro Kato"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981470161183360","@type":"Researcher","foaf:name":[{"@value":"Shigeru Kasuga"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00253235"},{"@type":"EISSN","@value":"15730581"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/00253235"}],"prism:publicationName":[{"@value":"Marine Geophysical Researches"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2001-01","prism:volume":"22","prism:number":"1","prism:startingPage":"47","prism:endingPage":"61"},"reviewed":"false","dc:rights":["https://www.springernature.com/gp/researchers/text-and-data-mining","https://www.springernature.com/gp/researchers/text-and-data-mining"],"url":[{"@id":"https://link.springer.com/content/pdf/10.1023/A:1004818225642.pdf"},{"@id":"https://link.springer.com/article/10.1023/A:1004818225642/fulltext.html"}],"createdAt":"2002-12-21","modifiedAt":"2025-07-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050564288827464192","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Amphibolitization within the lower crust in the termination area of the Godzilla Megamullion, an oceanic core complex in the Parece Vela Basin"},{"@value":"Amphibolitization within the lower crust in the termination area of the Godzilla Megamullion, Parece Vela backarc basin"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215039963392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tectonics of Unusual Crustal Accretion in the Parece Vela Basin"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002218164301440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"New insights on the origin of troctolites from the breakaway area of the Godzilla Megamullion (Parece Vela back‐arc basin): The role of melt‐mantle interaction on the composition of the lower crust"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002218474710656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Termination of backarc spreading: Zircon dating of a giant oceanic core complex"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229801443840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Curved grooves at the Godzilla Megamullion in the Philippine Sea and their tectonic significance"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004235528040320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Virtual special issue: Understanding of the largest oceanic core complex on the Earth, Godzilla Megamullion"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005517102445952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Melt–fluid infiltration along detachment shear zones in oceanic core complexes: Insights from amphiboles in gabbro mylonites from the Godzilla Megamullion, Parece Vela Basin, the Philippine Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283693141006976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Godzilla Megamullion, the largest oceanic core complex on the earth: a historical review"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285712684819072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"International Ocean Discovery Program Expedition 370 Preliminary Report Temperature Limit of the Deep Biosphere off Muroto"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565164993384704","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seafloor Geology of the Basement Serpentinite Body in the Ohmachi Seamount (Izu-Bonin Arc) as Exhumed Parts of a Subduction Zone Within the Philippine Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118702019840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Melting and Evolution of Amphibole‐Rich Back‐Arc Abyssal Peridotites at the Mado Megamullion, Shikoku Basin"}]},{"@id":"https://cir.nii.ac.jp/crid/1360583258211380992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geophysical investigation of the Mado Megamullion oceanic core complex: implications for the end of back-arc spreading"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640991983872","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Deformation and hydrothermal metamorphism of gabbroic rocks within the Godzilla Megamullion, Parece Vela Basin, Philippine Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848660458119936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The effect of a hydrous phase on P‐wave velocity anisotropy within a detachment shear zone in the slow‐spreading oceanic crust: A case study from the Godzilla Megamullion, Philippine Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848660540812544","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Relicts of deformed lithospheric mantle within serpentinites and weathered peridotites from the Godzilla Megamullion, Parece Vela Back‐arc Basin, Philippine Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567584972928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Crustal Accretion in a Slow Spreading Back‐Arc Basin: Insights From the Mado Megamullion Oceanic Core Complex in the Shikoku Basin"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869856050717824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Intact Pacific oceanic crust captured as mafic xenoliths in a petit-spot volcano"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204228572288","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Physical and Chemical Diversity of Seafloor Hydrothermal Systems and Presentation of Associated Chemolithoautotrophic Ecosystem"},{"@language":"ja","@value":"海底熱水系の物理・化学的多様性と化学合成微生物生態系の存在様式"},{"@language":"ja-Kana","@value":"カイテイ ネッスイケイ ノ ブツリ カガクテキ タヨウセイ ト カガク ゴウセイ ビセイブツ セイタイケイ ノ ソンザイ ヨウシキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204236635776","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"フィリピン海の磁気異常とテクトニクス"},{"@language":"en","@value":"Magnetic Anomalies in the Philippine Sea: Implications for Regional Tectonics"},{"@language":"ja-Kana","@value":"フィリピンカイ ノ ジキ イジョウ ト テクトニクス"},{"@value":"Magnetic anomalies in the Philippine Sea: implications for regional tectonics [in Japanese with English abstract]"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204236637056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"大陸棚調査が明らかにした日本南方海域海底の地球科学的特徴"},{"@language":"en","@value":"Geoscientific Characteristics of the Seafloor of the Southern Ocean of Japan Revealed by Japan's Continental Shelf Survey"},{"@language":"ja-Kana","@value":"タイリクダナ チョウサ ガ アキラカ ニ シタ ニホン ナンポウ カイイキ カイテイ ノ チキュウ カガクテキ トクチョウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206526290304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Petrography and Geochemistry of the mantle xenoliths: Implications for lithospheric mantle beneath the Japan arcs"},{"@language":"ja","@value":"かんらん岩捕獲岩の記載岩石化学的性質：日本列島下のリソスフェリック・マントルの特徴"},{"@value":"かんらん岩捕獲岩石の記載岩石化学的性質:日本列島下のリソスフェリック・マントルの特徴"},{"@language":"ja-Kana","@value":"カンランガン ホカク ガンセキ ノ キサイ ガンセキ カガクテキ セイシツ ニホン レットウ カ ノ リソスフェリック マントル ノ トクチョウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390009225704418048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Petrologic characteristics of the upper mantle beneath island arcs"},{"@language":"ja","@value":"島弧上部マントルの岩石学的性質: 何が固有か?"},{"@language":"ja-Kana","@value":"トウコ ジョウブ マントル ノ ガンセキガクテキ セイシツ : ナニ ガ コユウ カ?"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679206694528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Variations of Chemical Compositions of Mid-ocean Ridge Basalts (MORB) and their Origin"},{"@language":"ja","@value":"中央海嶺玄武岩（ＭＯＲＢ）の化学組成の多様性とその成因"},{"@value":"中央海嶺玄武岩の化学組成の多様性とその成因"},{"@language":"ja-Kana","@value":"チュウオウ カイレイ ゲンブガン ノ カガク ソセイ ノ タヨウセイ ト ソノ セイイン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679207022208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Crustal Lithology and Stratigraphy of Remnant Arcs Induced from Ophiolitic Rocks in the Idonnappu Zone Acceretionary Complex (Hokkaido,Japan): Comparison with Philippine Sea Remnant Arcs"},{"@value":"北海道イドンナップ帯付加体中のオフィオライトからみた残存島弧の地殻構成と層序―フィリピン海残存島弧との比較―"},{"@language":"ja-Kana","@value":"ホッカイドウ イドンナップタイ フカタイ チュウ ノ オフィオライト カラ ミタ ザンソントウ コ ノ チカク コウセイ ト ソウ ジョ フィリピンカイ ザンソントウ コ ト ノ ヒカク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680161378944","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"鋼溶接部の組織形成と制御"},{"@language":"en","@value":"Microstructure Development and Control in Steel Welds"},{"@value":"溶接・接合 鋼溶接部の組織形成と制御"},{"@language":"ja-Kana","@value":"ヨウセツ セツゴウ コウ ヨウセツブ ノ ソシキ ケイセイ ト セイギョ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681214064640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"New insights into the oceanic lithosphere from petit-spot volcanoes and “Super-Mohole” project"},{"@language":"ja","@value":"プチスポット火山から期待される海洋リソスフェアの包括的理解と地質学の新展開－超モホール計画の提案－"},{"@language":"ja-Kana","@value":"プチスポット カザン カラ キタイ サレル カイヨウ リソスフェア ノ ホウカツテキ リカイ ト チシツガク ノ シン テンカイ チョウモホール ケイカク ノ テイアン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390570950856456320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"IODP Drilling at the Godzilla Megamullion: The Nature of the Backarc Basin Lower Crust and Upper Mantle"},{"@language":"ja","@value":"ゴジラメガムリオン掘削から明らかにする背弧海盆海洋下部地殻と上部マントルの組成と構造"},{"@language":"ja-Kana","@value":"ゴジラメガムリオン クッサク カラ アキラカ ニ スル ハイ コカイボン カイヨウ カブ チカク ト ジョウブ マントル ノ ソセイ ト コウゾウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1570572701021321344","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Thematic Section : Geology and geophysics of the Philippine Sea and adjacent areas in the Pacific Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1570854175998124800","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seismic study on oceanic core complexes in the Parece Vela back-arc basin"}]},{"@id":"https://cir.nii.ac.jp/crid/1571135650974740992","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Variation of crustal thickness in the Philippine Sea deduced from three-dimensional gravity modeling"}]},{"@id":"https://cir.nii.ac.jp/crid/1573950400741848320","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fault configuration produced by initial arc rifting in the Parece Vela Basin as deduced from seismic reflection data"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317037091072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geochemical characteristics of back-arc basin lower crust and upper mantle at final spreading stage of Shikoku Basin : an example of Mado Megamullion"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317037095168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Peridotites with back-arc basin affinity exposed at the southwestern tip of the Mariana forearc"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317043074688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Lithological structure of western Pacific lithosphere reconstructed from mantle xenoliths in a petit-spot volcano"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1023/a:1004818225642"},{"@type":"CIA","@value":"30012562677"},{"@type":"CROSSREF","@value":"10.1007/978-90-481-8885-7_7_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.1111/iar.12137_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.1130/g31322.1_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.1002/2013tc003515_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.1111/iar.12157_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.2355/tetsutohagane1955.90.2_61_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.1186/s40645-022-00476-5_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.1186/s40645-022-00518-y_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.1186/s40645-023-00570-2_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.1111/iar.12116_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.1111/j.1440-1738.2010.00741.x_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.14379/iodp.pr.370.2017_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.2465/gkk.34.143_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2017.0037_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.1007/978-90-481-8885-7_5_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.5026/jgeography.124.687_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.5575/geosoc.116.1_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.5026/jgeography.130.543_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.1029/2021gc010013_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.1186/s40645-021-00454-3_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.1111/iar.12132_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.1111/j.1440-1738.2011.00759.x_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.5026/jgeography.117.124_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.5026/jgeography.118.1083_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.1029/2020gc009199_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.1016/j.margeo.2025.107497_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.1016/j.lithos.2019.06.019_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.1016/j.lithos.2011.02.001_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"},{"@type":"CROSSREF","@value":"10.5026/jgeography.124.729_references_DOI_Y5qp7LvpIWTR8FVm4bTsw2Ndlld"}]}