{"@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/1363388844968196992.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/91rg00969"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F91RG00969"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/91RG00969"}},{"identifier":{"@type":"NAID","@value":"30034661479"}}],"dc:title":[{"@value":"Observations at convergent margins concerning sediment subduction, subduction erosion, and the growth of continental crust"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>At ocean margins where two plates converge, the oceanic plate sinks or is subducted beneath an upper one topped by a layer of terrestrial crust. This crust is constructed of continental or island arc material. The subduction process either builds juvenile masses of terrestrial crust through arc volcanism or new areas of crust through the piling up of accretionary masses (prisms) of sedimentary deposits and fragments of thicker crustal bodies scraped off the subducting lower plate. At convergent margins, terrestrial material can also bypass the accretionary prism as a result of sediment subduction, and terrestrial matter can be removed from the upper plate by processes of subduction erosion. Sediment subduction occurs where sediment remains attached to the subducting oceanic plate and underthrusts the seaward position of the upper plate's resistive buttress (backstop) of consolidated sediment and rock. Sediment subduction occurs at two types of convergent margins: type 1 margins where accretionary prisms form and type 2 margins where little net accretion takes place. At type 2 margins (∼19,000 km in global length), effectively all incoming sediment is subducted beneath the massif of basement or framework rocks forming the landward trench slope. At accreting or type 1 margins, sediment subduction begins at the seaward position of an active buttress of consolidated accretionary material that accumulated in front of a starting or core buttress of framework rocks. Where small‐to‐medium‐sized prisms have formed (∼16,300 km), approximately 20% of the incoming sediment is skimmed off a detachment surface or decollement and frontally accreted to the active buttress. The remaining 80% subducts beneath the buttress and may either underplate older parts of the frontal body or bypass the prism entirely and underthrust the leading edge of the margin's rock framework. At margins bordered by large prisms (∼8,200 km), roughly 70% of the incoming trench floor section is subducted beneath the frontal accretionary body and its active buttress. In rounded figures the contemporary rate of solid‐volume sediment subduction at convergent ocean margins (∼43,500 km) is calculated to be 1.5 km³/yr. Correcting type 1 margins for high rates of terrigenous seafloor sedimentation during the past 30 m.y. or so sets the long‐term rate of sediment subduction at 1.0 km³/yr. The bulk of the subducted material is derived directly or indirectly from continental denudation. Interstitial water currently expulsed from accreted and deeply subducted sediment and recycled to the ocean basins is estimated at 0.9 km³/yr. The thinning and truncation caused by subduction erosion of the margin's framework rock and overlying sedimentary deposits have been demonstrated at many convergent margins but only off northern Japan, central Peru, and northern Chile has sufficient information been collected to determine average or long‐term rates, which range from 25 to 50 km³/m.y. per kilometer of margin. A conservative long‐term rate applicable to many sectors of convergent margins is 30 km³/km/m.y. If applied to the length of type 2 margins, subduction erosion removes and transports approximately 0.6 km³/yr of upper plate material to greater depths. At various places, subduction erosion also affects sectors of type 1 margins bordered by small‐ to medium‐sized accretionary prisms (for example, Japan and Peru), thus increasing the global rate by possibly 0.5 km³/yr to a total of 1.1 km³/yr. Little information is available to assess subduction erosion at margins bordered by large accretionary prisms. Mass balance calculations allow assessments to be made of the amount of subducted sediment that bypasses the prism and underthrusts the margin's rock framework. This subcrustally subducted sediment is estimated at 0.7 km³/yr. Combined with the range of terrestrial matter removed from the margin's rock framework by subduction erosion, the global volume of subcrustally subducted material is estimated to range from 1.3 to 1.8 km³/yr. Subcrustally subducted material is either returned to the terrestrial crust by arc‐related igneous processes or crustal underplating or is lost from the crust by mantle absorption. Geochemical and isotopic data support the notion that upper mantle melting returns only a small percent of the subducted material to the terrestrial crust as arc igneous rocks. Limited areal exposures of terrestrial rocks metamorphosed at deep (>20–30 km) subcrustal pressures and temperatures imply that only a small fraction of subducted material is reattached via deep crustal underplating. Possibly, therefore much of the subducted terrestrial material is recycled to the mantle at a rate near 1.6 km³/yr, which is effectively equivalent to the commonly estimated rate at which the mantle adds juvenile igneous material to the Earth's layer of terrestrial rock.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383388844968196992","@type":"Researcher","foaf:name":[{"@value":"Roland von Huene"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844968196993","@type":"Researcher","foaf:name":[{"@value":"David W. Scholl"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"87551209"},{"@type":"EISSN","@value":"19449208"}],"prism:publicationName":[{"@value":"Reviews of Geophysics"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1991-08","prism:volume":"29","prism:number":"3","prism:startingPage":"279","prism:endingPage":"316"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F91RG00969"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/91RG00969"}],"createdAt":"2008-02-06","modifiedAt":"2023-09-23","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282810757340928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Granular experiments of thrust wedges: Insights relevant to methane hydrate exploration at the Nankai accretionary prism"}]},{"@id":"https://cir.nii.ac.jp/crid/1050587981431983232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Hydrogeological responses to incoming materials at the erosional subduction margin, offshore Osa Peninsula, Costa Rica"},{"@value":"Hydrogeological responses to incoming materials at the erosional subduction margin, offshore <scp>O</scp>sa <scp>P</scp>eninsula, <scp>C</scp>osta <scp>R</scp>ica"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215942315520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The naked planet Earth: Most essential pre-requisite for the origin and evolution of life"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216044476800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Cambrian plutonism in Northeast Japan and its significance for the earliest arc-trench system of proto-Japan: New U–Pb zircon ages of the oldest granitoids in the Kitakami and Ou Mountains"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002218474767616","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tectonic erosion in a Pacific-type orogen: Detrital zircon response to Cretaceous tectonics in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002220102785280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Data report: compressional wave velocity measurements on sediments from the reference site off Kumano, Nankai Trough, NantroSEIZE Expedition 333"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229805467520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Volatile element isotopes of submarine hydrothermal mineral deposits in the Western Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232173836928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Cambrian Explosion: Plume-driven birth of the second ecosystem on Earth"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232324688896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismic imaging of the Asian orogens and subduction zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233285486592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Nitrogen sources and recycling at subduction zones: Insights from the Izu‐Bonin‐Mariana arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233286573824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Velocity‐porosity relationships for slope apron and accreted sediments in the Nankai Trough Seismogenic Zone Experiment, Integrated Ocean Drilling Program Expedition 315 Site C0001"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233481900800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Nitrogen recycling at the Costa Rican subduction zone: The role of incoming plate structure"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004235528229248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Material recycling in a sediment‐starved trench recorded in the Early Cretaceous Shiriya accretionary complex, Northeast Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142748431872","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Lattice preferred orientation of stishovite deformed at high pressure and high temperature"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017282189422848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evidence for Deeply Subducted Lower‐Plate Seamounts at the Hikurangi Subduction Margin: Implications for Seismic and Aseismic Behavior"}]},{"@id":"https://cir.nii.ac.jp/crid/1360019688963843072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ordovician Japan: geotectonic setting and palaeogeography"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025431093201664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Along-strike forearc and subducted upper slab structure beneath north Chile: Slow slip implications"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691021174272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mid-Paleozoic arc granitoids in SW Japan with Neoproterozoic xenocrysts from South China: New zircon U–Pb ages by LA-ICP-MS"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704780332160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Horizontal principal stress orientation in the Costa Rica Seismogenesis Project (CRISP) transect from borehole breakouts"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704786011904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Forearc Basin Stratigraphy and Interactions With Accretionary Wedge Growth According to the Critical Taper Concept"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707150544768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mantle convection with continental drift and heat source around the mantle transition zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707329514368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The role of compaction contrasts in sediments in décollement initiation in an accretionary prism"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285710979119104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rapid pulses of uplift, subsidence, and subduction erosion offshore Central America: Implications for building the rock record of convergent margins"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643843359360","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geochemistry and Sr–Nd isotopic composition of meta-gabbros from the Omi serpentinite mélange, Niigata, SW Japan: Evidence for subduction erosion in an immature early Paleozoic arc-trench system in proto-Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302865747569024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Temporal Evolution of Island Arc Magmatism and Its Influence on Long-Term Climate: Insights From the Izu Intra-Oceanic Arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166128818048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Generation of hydrous-carbonated plumes in the mantle transition zone linked to tectonic erosion and subduction"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166662444032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Quantifying crustal extension and shortening in the back‐arc region of Northeast Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166760580608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tsunamigenic potential of the shallow subduction plate boundary inferred from slow seismic slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182088656640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Silica diagenesis and its effect on interplate seismicity in cold subduction zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182127438976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The second continent: Existence of granitic continental materials around the bottom of the mantle transition zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567187579035008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evaluation of nutrient and energy sources of the deepest known serpentinite-hosted ecosystem using stable carbon, nitrogen, and sulfur isotopes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360568465785932672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Structural-morphological and sedimentary features of forearc slope off Miyagi, NE Japan: implications for development of forearc basins and plumbing systems"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640867369984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The contribution of hydrothermally altered ocean crust to the mantle halogen and noble gas cycles"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640872466432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Hadean Earth and primordial continents: The cradle of prebiotic life"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640974527872","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Recognition of the Shimanto HP metamorphic belt within the traditional Sanbagawa HP metamorphic belt: New perspectives of the Cretaceous–Paleogene tectonics in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654731567872","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Long-term evolution of an accretionary prism: The case study of the Shimanto Belt, Kyushu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654739409408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tertiary evolution of the Shimanto belt (Japan): A large‐scale collision in Early Miocene"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848655105773824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Time‐averaged SO<sub>2</sub> fluxes of subduction‐zone volcanoes: Example of a 32‐year exhaustive survey for Japanese volcanoes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657065384320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Runaway slip to the trench due to rupture of highly pressurized megathrust beneath the middle trench slope: The tsunamigenesis of the 2011 Tohoku earthquake off the east coast of northern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657104179200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Why primordial continents were recycled to the deep: Role of subduction erosion"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657104193408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High-pressure phase transitions of anorthosite crust in the Earth's deep mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657453484416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Supply rate of continental materials to the deep mantle through subduction channels"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657453635712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Organic matter cracking: A source of fluid overpressure in subducting sediments"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848660458457600","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A visage of early Paleozoic Japan: Geotectonic and paleobiogeographical significance of Greater South China"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848663510499968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Data report: compressional and shear wave velocity measurements on sediment in the hanging wall and footwall of megasplay fault, NanTroSEIZE Stage 1"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861287035222144","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geodetic and Geological Deformation of the Island Arc in Northeast Japan Revealed by the 2011 Tohoku Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360862720784932224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Clockwise rotation of SW Japan and timing of Izanagi–Pacific ridge subduction revealed by arc migration"}]},{"@id":"https://cir.nii.ac.jp/crid/1361131418080329600","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Control of Fault Weakening on the Structural Styles of Underthrusting‐Dominated Non‐Cohesive Accretionary Wedges"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994152614400","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@value":"Anatomy and genesis of a subduction‐related orogen: A new view of geotectonic subdivision and evolution of the Japanese Islands"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204062072064","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"アナログモデル実験で再現された付加体構造に対する反射法地震探査記録の合成"},{"@language":"en","@value":"Synthetic seismic sections of an accretionary prism reproduced by 3D sandbox experiment"},{"@language":"ja-Kana","@value":"アナログ モデル ジッケン デ サイゲンサレタ フカタイ コウゾウ ニ タイスル ハンシャホウ ジシン タンサ キロク ノ ゴウセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204228786688","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Opening of Japan Sea and Major Tectonic Lines of Japan"},{"@value":"日本海の拡大と構造線"},{"@language":"ja-Kana","@value":"ニホンカイ ノ カクダイ ト コウゾウセン MTL TTL ソシテ フォッサマグナ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204228970752","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Various Perspectives on Accretionary Wedge Formation and Related Phenomena"},{"@value":"付加体形成をめぐる諸問題"},{"@language":"ja-Kana","@value":"チガク クラブ コウエン ホウコク フカタイ ケイセイ オ メグル ショモンダイ ミカイケツ ノ モンダイ ト ジュウリョク ノ ヤクワリ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204229563008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"太平洋型造山帯"},{"@language":"en","@value":"Pacific-type Orogens"},{"@value":"太平洋型造山帯--新しい概念の提唱と地球史における時空分布"},{"@language":"ja-Kana","@value":"タイヘイヨウガタ ゾウザンタイ アタラシイ ガイネン ノ テイショウ ト チキュウシ ニ オケル ジクウ ブンプ"},{"@value":"Pacific type Orogens: new concepts and variations in space and time from present to past"},{"@value":"Pacific-type Orogens: new concepts and variations in space and time from present to past (in Japanese with English abstract)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204230429440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"At the Stage of \"Exporting Science\": A Historical Review of Studies on the Geotectonic Subdivision and Orogeny of the Japanese Islands"},{"@language":"ja","@value":"輸出科学の時代―日本列島の地体構造区分・造山運動研究史―"},{"@language":"ja-Kana","@value":"ユシュツ カガク ノ ジダイ ニホン レットウ ノ チタイ コウゾウ クブン ゾウザン ウンドウ ケンキュウシ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204230813184","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tectonic Erosion: New Perspectives on Pacific-type Orogeny and Continental Growth Models"},{"@language":"ja","@value":"構造浸食作用―太平洋型造山運動論と大陸成長モデルへの新視点―"},{"@language":"ja-Kana","@value":"コウゾウ シンショク サヨウ タイヘイヨウガタ ゾウザン ウンドウロン ト タイリク セイチョウ モデル エ ノ シン シテン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204230827776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Second Continent"},{"@language":"ja","@value":"第２大陸"},{"@language":"ja-Kana","@value":"ダイ2 タイリク"},{"@value":"The second continent (in Japanese with English abstract)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204237574144","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Classification of Orogenic Belts: Constraints on the Reconstruction of Paleo-geotectonic Environments"},{"@language":"ja","@value":"造山帯の分類とその意義：古造構場復元の束縛条件"},{"@value":"造山帯の分類とその意義 : 古造構場復元の束縛条件 : 「丸山ほか : 太平洋型造山帯 : 新しい概念の提唱と地球史における時空分布」論文(地学雑誌,120巻,115-223)の追記"},{"@language":"ja-Kana","@value":"ゾウザンタイ ノ ブンルイ ト ソノ イギ : コゾウコウジョウ フクゲン ノ ソクバク ジョウケン : 「 マルヤマ ホカ : タイヘイヨウガタ ゾウザンタイ : アタラシイ ガイネン ノ テイショウ ト チキュウシ ニ オケル ジクウ ブンプ 」 ロンブン(チガク ザッシ,120カン,115-223)ノ ツイキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204238418944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"地球型惑星内部物理学の最近の進展"},{"@language":"en","@value":"Recent Advances in Geophysical Studies of the Interior of Terrestrial Planets"},{"@language":"ja-Kana","@value":"チキュウガタ ワクセイ ナイブ ブツリガク ノ サイキン ノ シンテン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204307265408","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"震度分布による津波地震の一判別法"},{"@language":"en","@value":"A Judging Method of Tsunami Earthquake from Seismic Intensity Distribution"},{"@value":"震度分布による津波地震の一判別法--日本付近における津波地震の分布"},{"@language":"ja-Kana","@value":"シンド ブンプ ニヨル ツナミ ジシン ノ イチハンベツホウ ニホン フキン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205417980928","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Influences of Material Properties on Analogue Model Experiments of Geologic Structures"},{"@language":"ja","@value":"地質構造形成過程のアナログモデル実験における材料物性の影響"},{"@language":"ja-Kana","@value":"チシツ コウゾウ ケイセイ カテイ ノ アナログ モデル ジッケン ニ オケル ザイリョウ ブッセイ ノ エイキョウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206238793856","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Analogue model experiments on the formation of accretionary prism"},{"@language":"ja","@value":"付加体形成過程のモデル実験"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288092674048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"地球史を通じた大陸の成長パターンとその変遷"},{"@language":"en","@value":"Pattern of Continental Growth and Its Secular Change"},{"@language":"ja-Kana","@value":"チキュウシ オ ツウジタ タイリク ノ セイチョウ パターン ト ソノ ヘンセン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679205505280","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Overview of a Special Issue on “Geotectonic Evolution of the Japanese Islands under New Paradigms of the Next Generation (Part I-III)”"},{"@value":"Overview of a special issue on \"geotectonic evolution of the Japanese Islands under new paradigms of the next generation (part 1-3)\""},{"@value":"Overview of a Special Issue on &ldquo;Geotectonic Evolution of the Japanese Islands under New Paradigms of the Next Generation (Part I-III)&rdquo;"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679206278656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Growth and Shrinkage of an Active Continental Margin: Updated Geotectonic History of the Japanese Islands"},{"@language":"ja","@value":"活動的大陸縁の肥大と縮小の歴史―日本列島形成史アップデイト―"},{"@language":"ja-Kana","@value":"カツドウテキ タイリクエン ノ ヒダイ ト シュクショウ ノ レキシ ニホン レットウ ケイセイシ アップデイト"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679207522048","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geotectonic Subdivision of the Japanese Islands Revisited: Categorization and Definition of Elements and Boundaries of Pacific-type (Miyashiro-type) Orogen"},{"@language":"ja","@value":"日本列島の地体構造区分再訪―太平洋型（都城型）造山帯構成単元および境界の分類・定義―"},{"@language":"ja-Kana","@value":"ニホン レットウ ノ ジタイ コウゾウ クブン サイホウ タイヘイヨウガタ ミヤシロガタ ゾウザンタイ コウセイ タンゲン オヨビ キョウカイ ノ ブンルイ テイギ"},{"@value":"Geotectonic subdivision of the Japanese Islands revisited: Categorization and definition of elements and boundaries of Pacific-type (Miyashiro-type) orogeny"},{"@value":"Geotectonic subdivision of the Japanese Islands revisited and relevant new perspective: categorization and definition of elements and boundaries of a Pacific-type (Miyashiro-type) orogen"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679207539072","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Have the Japanese Islands Grown?: Five \"Japan\"s Were Born, and Four \"Japan\"s Subducted into the Mantle"},{"@language":"ja","@value":"日本列島の大陸地殻は成長したのか？―５つの日本が生まれ，４つの日本が沈み込み消失した―"},{"@language":"ja-Kana","@value":"ニホン レットウ ノ タイリク チカク ワ セイチョウ シタ ノ カ イツツ ノ ニホン ガ ウマレ ヨッツ ノ ニホン ガ シズミ コミ ショウシツ シタ"},{"@value":"Have the Japanese islands grown?: five “Japan”s were born, and four “Japan”s were subducted into the mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679213860736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"マントル物質のハロゲン組成にみられるスラブ起源流体の痕跡"},{"@language":"en","@value":"Traces of Slab-derived Fluids Revealed by Halogens in Mantle-derived Rocks"},{"@language":"ja-Kana","@value":"マントル ブッシツ ノ ハロゲン ソセイ ニ ミラレル スラブ キゲン リュウタイ ノ コンセキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679527154432","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Role of subducted sediments in the genesis of Kurile-Kamchatka island arc basalts: Sr isotopic and elemental evidence."},{"@language":"ja-Kana","@value":"Role of subducted sediments in the gene"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679530771200","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Low ratio of sediment recycling at Northeast Japan Arc: Constraints from <sup>10</sup>Be isotopes and B-Ba-K-Be systematics"},{"@value":"Low ratio of sediment recycling at Northeast Japan Arc : Constraints from ¹⁰Be isotopes and B-Ba-K-Be systematics"}]},{"@id":"https://cir.nii.ac.jp/crid/1390306672257570432","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"近畿地方北部の超丹波帯付加複合体における層序型の類別と付加環境の変遷"},{"@language":"en","@value":"Categorization of stratigraphic types in the accretionary complex within the Ultra-Tamba Belt, northern Kinki district, Southwest Japan: A transition in accretionary environment"},{"@language":"ja-Kana","@value":"キンキ チホウ ホクブ ノ チョウタンバタイ フカ フクゴウタイ ニ オケル ソウ ジョガタ ノ ルイベツ ト フカ カンキョウ ノ ヘンセン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390848250127877632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Secular Changes in Fore-arc Sandstones and Their Provenance in Cretaceous Southwest Japan: U–Pb Dating of Detrital Zircons"},{"@language":"ja","@value":"白亜紀西南日本の前弧砂岩と後背地の経年変化"},{"@value":"白亜紀西南日本の前弧砂岩と後背地の経年変化 : 砕屑性ジルコンのU-Pb年代測定"},{"@language":"ja-Kana","@value":"ハクアキ セイナン ニホン ノ ゼン コ サガン ト コウハイチ ノ ケイ ネンヘンカ : サイクズセイ ジルコン ノ U-Pb ネンダイ ソクテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1520572360202301568","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@value":"日本列島の起源と付加型造山帯の成長--リフト帯での誕生から都城型造山運動へ"},{"@language":"ja-Kana","@value":"ニホン レットウ ノ キゲン ト フカガタ ゾウザンタイ ノ セイチョウ リフトタイ デ ノ タンジョウ カラ トジョウガタ ゾウザン ウンドウ エ"},{"@language":"en","@value":"Origin and growth of accretionary orogen of the Japanese Islands : From birth at rift zone to Miyashiro-type orogeny"}]},{"@id":"https://cir.nii.ac.jp/crid/1570009749568789376","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The 1992 Sanriku-Oki, Japan, Ultra-Slow Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1570854176026888832","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Across-arc geochemical variation of Quaternary lavas in West Java, Indonesia : Mass-balance elucidation using arc basalt simulator model"}]},{"@id":"https://cir.nii.ac.jp/crid/1573668924962374272","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"砂箱実験で再現された付加体構造に対する反射法地震探査記録の合成"},{"@language":"en","@value":"Synthetic reflection seismic data for 3D sandbox experiment of accretionary prism"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317070231936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geotechnical behavior of mudstones from the Shimanto and Boso accretionary complexes, and implications for the Nankai accretionary prism"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/91rg00969"},{"@type":"CIA","@value":"30034661479"},{"@type":"CROSSREF","@value":"10.1130/g33414.1_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1002/2016gc006360_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1029/2009gc002783_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1029/2010gc003217_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1038/s41598-017-14287-y_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1111/iar.12272_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.5026/jgeography.120.115_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2016.03.014_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2012.04.002_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.5026/jgeography.119.1173_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.2343/geochemj.2.0468_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.gsf.2017.10.002_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.marpetgeo.2013.11.008_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.jseaes.2017.06.016_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2020.106546_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1029/2021jb022866_references_DOI_8sp9Eg0P2SnJv9TkrTzjb4bcTR1"},{"@type":"CROSSREF","@value":"10.1186/s40645-023-00594-8_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.9795/bullgsj.76.6_313_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.jsames.2024.105064_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1002/2015gc006092_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1002/2017tc004744_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1130/g34355.1_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.5026/jgeography.119.1079_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.5026/jgeography.119.999_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.gr.2013.03.013_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.5026/jgeography.119.153_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.5026/jgeography.121.1090_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.margeo.2011.02.011_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.lithos.2021.106260_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.3389/feart.2022.810597_references_DOI_8sp9Eg0P2SnJv9TkrTzjb4bcTR1"},{"@type":"CROSSREF","@value":"10.1029/2011jb008355_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1038/ngeo1466_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1371/journal.pone.0199000_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.2204/iodp.proc.333.202.2014_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1007/s00367-020-00636-w_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.gsf.2016.07.005_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.jseaes.2014.10.018_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2013.02.001_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2017.08.005_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.5026/jgeography.119.963_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.2472/jsms.55.452_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.5026/jgeography.120.65_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.gr.2013.02.001_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-129_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1144/sp533-2022-80_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1002/2013tc003412_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1002/2015gc005837_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1002/2017tc004529_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1002/jgrd.50591_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1111/iar.12296_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.2204/iodp.proc.314315316.217.2011_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.5026/jgeography.119.1197_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.5026/jgeography.119.378_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.5575/geosoc.112.s153_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2015.08.005_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1146/annurev-earth-032320-074429_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.gsf.2016.08.001_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1029/2019jb019220_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.5026/jgeography.127.705_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.5026/jgeography.124.445_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.3720/japt.72.279_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.jseaes.2011.05.001_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.5026/jgeography.119.947_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.jseaes.2015.04.024_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.gsf.2012.11.001_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.5026/jgeography.124.1_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2011.11.041_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.1016/j.gsf.2012.08.003_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"},{"@type":"CROSSREF","@value":"10.5026/jgeography.129.397_references_DOI_ZUmwGqSuPksRzjRRgXAYUOqtmJs"}]}