{"@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/1360574095468024576.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.pepi.2010.02.004"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0031920110000300?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0031920110000300?httpAccept=text/plain"}}],"dc:title":[{"@value":"The global range of subduction zone thermal models"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380574095468024448","@type":"Researcher","foaf:name":[{"@value":"Ellen M. Syracuse"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574095468024449","@type":"Researcher","foaf:name":[{"@value":"Peter E. van Keken"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574095468024576","@type":"Researcher","foaf:name":[{"@value":"Geoffrey A. Abers"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00319201"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/00319201"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/00319201"}],"prism:publicationName":[{"@value":"Physics of the Earth and Planetary Interiors"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2010-11","prism:volume":"183","prism:number":"1-2","prism:startingPage":"73","prism:endingPage":"90"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0031920110000300?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0031920110000300?httpAccept=text/plain"}],"createdAt":"2010-02-15","modifiedAt":"2023-05-30","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050013861703678720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Temperature distribution for interplate seismic events in the southcentral Alaska subduction zone based on 3-D thermomechanical modeling"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002218474789504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Plate tectonic gemstones"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229801701248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Along‐arc variation in the 3‐D thermal structure around the junction between the Japan and Kurile arcs"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229805679232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sound velocities of aluminum‐bearing stishovite in the mantle transition zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004230122316544","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Two‐dimensional viscosity structure of the northeastern Japan islands arc‐trench system"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232051056128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effect of the volcanic front migration on helium, nitrogen, argon, and carbon geochemistry of hydrothermal/magmatic fluids from Hokkaido volcanoes, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232135202304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermodynamic forward modeling of progressive dehydration reactions during subduction of oceanic crust under greenschist facies conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232349744128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effect of water on the magnesite–iron interaction, with implications for the fate of carbonates in the deep mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232425600512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Equation of state and phase transition of antigorite under high pressure and high temperature"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232425641344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The CaCO3–Fe interaction: Kinetic approach for carbonate subduction to the deep Earth’s mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232456348416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Constraints on the P–T conditions of high-pressure metamorphic rocks from the Inyoni shear zone in the mid-Archean Barberton Greenstone Belt, South Africa"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004235781788288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Lawsonite blueschists and lawsonite eclogites as proxies for palaeo‐subduction zone processes: a review"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004240202138112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermal structure and intermediate-depth seismicity in the Tohoku-Hokkaido subduction zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005518352195712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Saline aqueous fluid circulation in mantle wedge inferred from olivine wetting properties"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142888763008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Slow Earthquakes Illuminating Interplate Coupling Heterogeneities in Subduction Zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017282211975680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sulfur Isotope and Trace Element Systematics in Arc Magmas: Seeing through the Degassing via a Melt Inclusion Study of Kyushu Island Volcanoes, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021390560610048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Olivine-Hosted Melt Inclusions Track Progressive Dehydration Reactions in Subducting Slabs Across Volcanic Arcs"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025430667555968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Subduction of Hydrogen: Deep Water Cycling, Induced Seismicity, and Plate Tectonics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283689327092736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Origin of geochemical mantle components: Role of spreading ridges and thermal evolution of mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691123216640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Physicochemical conditions for melting in the Earth’s mantle containing a C–O–H fluid (from experimental data)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691152066304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rheological contrast between serpentine species and implications for slab–mantle wedge decoupling"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283693451611136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Breakdown of residual zircon in the Izu arc subducting slab during backarc rifting"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283693614078208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Jadeitites and Plate Tectonics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704779284736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Deformation microstructures of glaucophane and lawsonite in experimentally deformed blueschists: Implications for intermediate‐depth intraplate earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704782249856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Origin of ultra rear‐arc magmatism at <scp>R</scp>ishiri <scp>V</scp>olcano, <scp>K</scp>uril <scp>A</scp>rc"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285705152034816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Shear wave anisotropy beneath the volcanic front in South Kyushu area, Japan: Development of C‐type olivine CPO under H<sub>2</sub>O‐rich conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707143316736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Behaviour of subducted water and its role in magma genesis in the NE Japan arc: A combined geophysical and geochemical approach"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707150643200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geochemical mapping of slab-derived fluid and source mantle along Japan arcs"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707150758016","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Subduction of the primordial crust into the deep mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708266539648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Melt inclusions reveal geochemical cross‐arc variations and diversity within magma chambers feeding the Higashi‐Izu Monogenetic Volcano Field, Izu Peninsula, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708268904576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Aqueous Fluid Connectivity in Subducting Oceanic Crust at the Mantle Transition Zone Conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708445291520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rapid mantle flow with power-law creep explains deformation after the 2011 Tohoku mega-quake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708457079936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Genesis of ultra-high-Ni olivine in high-Mg andesite lava triggered by seamount subduction"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285710979299840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dehydration of phengite inferred by electrical conductivity measurements: Implication for the high conductivity anomalies relevant to the subduction zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617895443712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High nitrogen solubility in stishovite (SiO2) under lower mantle conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617903779840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A new concept for the genesis of felsic magma: the separation of slab-derived supercritical liquid"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643744267264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The thermal structure of subduction zones predicted by plate cooling models with variable thermal properties"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643801855872","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Chemical Stability of FeOOH at High Pressure and Temperature, and Oxygen Recycling in Early Earth History**"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643820198272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Late Jurassic adakite˗like granodiorite along the southern Karakoram block, NE Pakistan: New evidence for subduction initiation of the Neo-Tethys Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298754814832384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Large-scale structures in the Earth’s interior: Top-down hemispherical dynamics constrained by geochemical and geophysical approaches"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298754825724032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Low Thermal Conductivity of Hydrous Phase D Leads to a Self‐Preservation Effect Within a Subducting Slab"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298754829151360","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Melting of Fe-bearing and Fe-free carbonated pelites under fluid-saturated conditions at 6 GPa"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302864792640768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Partial Melting under Shallow-Crustal Conditions: A Study of the Pleistocene Caldera Eruption of Mendeleev Volcano, Southern Kuril Island Arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302864796231424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Deciphering Deep Mantle Processes from Isotopic and Highly Siderophile Element Compositions of Mantle‐Derived Rocks: Prospects and Limitations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302865745353856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Magnesian Andesites from Kibblewhite Volcano in the Kermadec Arc, New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1360305193162093184","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Subducted carbon weakens the forearc mantle wedge in a warm subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306904418153856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Significance of serpentinite‐hosted exhumation channels in a palaeo‐subduction complex, Nishisonogi unit, Nagasaki Metamorphic Complex: <i>P–T</i> trajectories of mélange blocks and coherent schists"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165262707712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Transition from dehydration to hydration during exhumation of the Sanbagawa metamorphic belt, Japan, revealed by the continuous P–T path recorded in garnet and amphibole zoning"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165869642496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermal–petrological controls on the location of earthquakes within subducting plates"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165997931776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tectonic implications of Early Miocene OIB magmatism in a near-trench setting: The Outer Zone of SW Japan and the northernmost Ryukyu Islands"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166067217152","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"P-V-T equation of state of CaCO3 aragonite to 29 GPa and 1673 K: In situ X-ray diffraction study"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166813842944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Diamond formation in the deep lower mantle: a high-pressure reaction of MgCO3 and SiO2"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179759802112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Estimate of subduction rate of island arcs to the deep mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567181183711232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evolution of carbon dioxide-bearing saline fluids in the mantle wedge beneath the Northeast Japan arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567181859862272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dynamics of Subducting Slabs: Numerical Modeling and Constraints from Seismology, Geoid, Topography, Geochemistry, and Petrology"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182088766976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Melting and subsolidus phase relations in peridotite and eclogite systems with reduced C O H fluid at 3–16 GPa"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182088843904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mantle wedge flow pattern and thermal structure in Northeast Japan: Effects of oblique subduction and 3-D slab geometry"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567188358222848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stability of the hydrous phases of Al-rich phase D and Al-rich phase H in deep subducted oceanic crust"}]},{"@id":"https://cir.nii.ac.jp/crid/1360568467151241088","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Fate of water in subducted hydrous sediments deduced from stability fields of FeOOH and AlOOH up to 20 GPa"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092548278272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electrical Conductivity in Texturally Equilibrated Fluid‐Bearing Forsterite Aggregates at 800°C and 1 GPa: Implications for the High Electrical Conductivity Anomalies in Mantle Wedges"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092838060672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stagnant forearc mantle wedge inferred from mapping of shear-wave anisotropy using S-net seafloor seismometers"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092857525248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Petrogenesis of the Higashi-Akaishi Ultramafic Body: Implications for Lower Crustal Foundering and Mantle Wedge Processes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118747835648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Shallow Slow Earthquake Episodes Near the Trench Axis off Costa Rica"}]},{"@id":"https://cir.nii.ac.jp/crid/1360579813376010624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High thermal conductivity of stishovite promotes rapid warming of a sinking slab in Earth's mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580229795932672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effect of Pressure on the Thermal Cracking and Polymerization of Pentacosane (<i>n</i>-C<sub>25</sub>), an <i>n</i>-Alkane"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580232138919552","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rheology of Naturally Deformed Antigorite Serpentinite: Strain and Strain‐Rate Dependence at Mantle‐Wedge Conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580232386592768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sanbe volcano: Long‐term evolution of an arc magmatic system"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584339753578496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Phase Relation and Equation of State of Iron‐Titanium Oxyhydroxides With α‐PbO<sub>2</sub> Type Crystal Structure at Deep Mantle Conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584341816281856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A review of shallow slow earthquakes along the Nankai Trough"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588380586980992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Crystallographic Preferred Orientation of Phase D at High Pressure and Temperature: Implications for Seismic Anisotropy in the Mid‐Mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846639280483200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Origin of geochemical mantle components: Role of subduction filter"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640787763200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Melting of dehydrated oceanic crust from the stagnant slab and of the hydrated mantle transition zone: Constraints from Cenozoic alkaline basalts in eastern China"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640846286720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The effect of sediment recycling in subduction zones on the Hf isotope character of new arc crust, Banda arc, Indonesia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846642062237184","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Separation of supercritical slab-fluids to form aqueous fluid and melt components in subduction zone magmatism"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654733823104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Slab‐derived fluids, fore‐arc hydration, and sub‐arc magmatism beneath Kyushu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657355731200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Deformation fabrics of natural blueschists and implications for seismic anisotropy in subducting oceanic crust"}]},{"@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/1360848658219977344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Across‐ and along‐arc geochemical variations of lava chemistry in the Sangihe arc: Various fluid and melt slab fluxes in response to slab temperature"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848659671877888","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High-Mg Adakite and Low-Ca Boninite from a Bonin Fore-arc Seamount: Implications for the Reaction between Slab Melts and Depleted Mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567524639104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Experimental constraint on grain-scale fluid connectivity in subduction zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567635232512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Semi-brittle deformation of antigorite serpentinite under forearc mantle wedge conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567814800000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The stability of subducted glaucophane with the Earth’s secular cooling"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593646689024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Partial dehydration of brucite and its implications for water distribution in the subducting oceanic slab"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593647143296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electrical conductivity of diaspore, δ-AlOOH and ε-FeOOH"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593684447232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A New Reference Model for the Evolution of Oceanic Lithosphere in a Cooling Earth"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593710927616","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Listvenite Formation During Mass Transfer into the Leading Edge of the Mantle Wedge: Initial Results from Oman Drilling Project Hole BT1B"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593756091392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effect of Water on Lattice Thermal Conductivity of Ringwoodite and Its Implications for the Thermal Evolution of Descending Slabs"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861705591779584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Interaction of carbonates with peridotite containing iron metal: Implications for carbon speciation in the upper mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861707157648384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Along-arc heterogeneous rheology inferred from post-seismic deformation of the 2011 Tohoku-oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861707393983488","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Pressure–temperature paths of tectonic blocks in mélange: Recording thermal evolution of a subduction channel at an initial stage of subduction"}]},{"@id":"https://cir.nii.ac.jp/crid/1360866922335563136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Role of water in dynamics of slabs and surrounding mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869454283768448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Limited stability of hydrous SiO2 stishovite in the deep mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869855108875392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Implications of Surface Heat Flux for Shear Stress and Temperature on the Plate Interface Beneath Northern Honshu"}]},{"@id":"https://cir.nii.ac.jp/crid/1361131417009270272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Boron isotope variations of Franciscan serpentinites, northern California"}]},{"@id":"https://cir.nii.ac.jp/crid/1361131418078834176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Two‐Dimensional Thermal Modeling of the Philippine Sea Plate Subduction in Central Japan: Implications for Gap of Low‐Frequency Earthquakes and Tectonic Tremors"}]},{"@id":"https://cir.nii.ac.jp/crid/1361131418079806976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Event Size Distribution of Shallow Tectonic Tremor in the Nankai Trough"}]},{"@id":"https://cir.nii.ac.jp/crid/1361131420852897792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Coupled afterslip and transient mantle flow after the 2011 Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1361412891725115008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evolution and maturation of the nascent Mariana arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204237163136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Chemical Composition of Mantle Wedge Fluids"},{"@language":"ja","@value":"マントルウェッジ流体の化学組成"},{"@language":"ja-Kana","@value":"マントルウェッジ リュウタイ ノ カガク ソセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206525456896","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Melt-peridotite reactions: Roles in magma genesis beneath mid-ocean ridges, oceanic islands, and volcanic arcs"},{"@language":"ja","@value":"メルト-かんらん岩反応：海嶺・海洋島・島弧マグマの成因に果たす役割"},{"@language":"ja-Kana","@value":"メルトー カンランガン ハンノウ : カイレイ ・ カイヨウトウ ・ トウコ マグマ ノ セイイン ニ ハタス ヤクワリ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206546109568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Morphological stability of hydrous liquid droplets at grain boundaries of eclogite minerals in the deep upper mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206546995456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Jadeitite (jadeite jade) from Japan: History, characteristics, and perspectives"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288126621184","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Retrograde pumpellyite in the Yunotani garnet blueschist of the Omi area, Japan: An update on the cooling path"}]},{"@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/1390282681523216768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Evidence of the lawsonite eclogite facies metamorphism from an epidote-glaucophane eclogite in the Kotsu area of the Sanbagawa belt, Japan"},{"@value":"Evdence of the lawsonite-eclogite facies metamorphism from an epidote-glaucophane eclogite in the Kotsu area of the Sanbagawa belt, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390305035470774912","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"長崎変成岩西彼杵ユニット中の蛇紋岩メランジュ：超高圧変成岩を含む雪浦メランジュとヒスイ輝石岩を産する三重メランジュ"},{"@language":"en","@value":"Serpentinite mélanges from the Nishisonogi unit, Nagasaki Metamorphic Complex: the Yukinoura mélange containing ultrahigh-pressure metamorphic rocks and the Mie mélange with jadeitites"}]},{"@id":"https://cir.nii.ac.jp/crid/1390570950855611264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Drilling into the Mantle: A Key to Prognosticating the Future of the Ocean Planet"},{"@language":"ja","@value":"海惑星の将来を考える"},{"@value":"海惑星の将来を考える : マントル掘削の意義"},{"@language":"ja-Kana","@value":"ウミ ワクセイ ノ ショウライ オ カンガエル : マントル クッサク ノ イギ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390587196512052992","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"地球深部における窒素の振る舞い–分化・貯蔵庫形成・供給過程–"},{"@language":"en","@value":"Behavior of Nitrogen in the Deep Earth–Process of Differentiation, Formation of Reservoir, and Transportation–"},{"@language":"ja-Kana","@value":"チキュウ シンブ ニ オケル チッソ ノ フルマイ : ブンカ ・ チョゾウコ ケイセイ ・ キョウキュウ カテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390845713053175040","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"数値モデルと観測との比較に基づく沈み込み帯ダイナミクスの解明"},{"@language":"en","@value":"Subduction Zone Dynamics Constrained from Numerical Models and Observations"},{"@language":"ja-Kana","@value":"スウチ モデル ト カンソク ト ノ ヒカク ニ モトズク シズミ コミ タイ ダイナミクス ノ カイメイ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367116788224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Numerical modeling of trace element transportation in subduction zones : implications for geofluid processes"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842066368640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Heterogeneous rheology of Japan subduction zone revealed by postseismic deformation of the 2011 Tohoku-oki earthquake"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.pepi.2010.02.004"},{"@type":"CROSSREF","@value":"10.1130/g34204.1_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1002/2014gc005394_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1002/2016gl068377_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1002/grl.50906_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1111/jmg.12057_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.5194/se-3-355-2012_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1038/s41467-019-13513-7_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2010.12.053_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.2465/gkk.120611b_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.2343/geochemj.2.0468_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2013.08.027_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2013.07.008_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1029/2020gl088089_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1093/petrology/egac061_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1093/petrology/egae017_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.5194/sed-4-1069-2012_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.2138/gselements.20.4.229_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1002/2016gc006696_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1130/g39856.1_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1002/2014jb011528_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1002/2016gc006594_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1002/jgrb.50300_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1029/2012gc004222_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1029/2018jb015973_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1038/s41467-019-08984-7_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1038/s41598-017-10276-3_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1130/g39716.1_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.gr.2019.01.007_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2017.02.006_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-26_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1038/s41598-020-67621-2_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1038/s41598-020-65641-6_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1093/gji/ggac008_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1002/ejic.202100274_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.lithos.2021.106496_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.3389/feart.2022.1033378_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1029/2022jb024556_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1093/petrology/egad025_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1093/petrology/egad033_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1002/9781119526919.ch5_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1093/petrology/egad060_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1111/iar.12527_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1007/s00410-015-1185-9_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1038/srep40602_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1002/2016jb013119_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1007/s00410-014-1056-9_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1146/annurev-earth-060614-105215_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.2138/am-2019-6559_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2015.06.021_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2017.08.005_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.lithos.2019.01.004_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1029/2020jb021343_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1038/s41467-020-19541-y_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1093/petrology/egaa089_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1029/2021jb021706_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2022.117477_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1021/acsearthspacechem.2c00235_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1029/2022gl098945_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1111/iar.12453_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1029/2023jb027906_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1186/s40645-023-00539-1_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1186/s40623-023-01920-6_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.4131/jshpreview.35.135_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1029/2024jb029734_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1002/2016gc006343_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1073/pnas.1207687109_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1002/2015gl063084_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1029/2012gc004346_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1093/petrology/egt008_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.rgg.2011.04.001_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2014.04.019_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.2465/jmps.121022b_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.gsf.2016.08.003_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.5026/jgeography.130.585_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2020.116610_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.jsg.2020.104151_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1038/s41467-021-21746-8_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.gsf.2021.101342_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.2138/am-2021-7605_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1029/2020jb021528_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1029/2020gl087607_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1029/2021jb022352_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.lithos.2022.106817_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1093/gji/ggac063_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1111/jmg.12718_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2022.229604_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2024.118790_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1029/2023gc011285_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1186/s40645-024-00670-7_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1038/s41467-024-51476-6_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2025.0018_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.2465/jmps.170804_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.lithos.2019.02.004_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2016.08.008_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1029/2018jb017068_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1029/2019gl083029_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1126/sciadv.aaw1164_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2019.115912_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.chemgeo.2015.08.006_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2013.06.011_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.2465/jmps.170309_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.5026/jgeography.124.473_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.chemgeo.2013.09.012_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.precamres.2018.06.018_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2011.01.027_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/b978-0-444-53802-4.00132-9_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.4294/zisin.2017-10_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2013.03.022_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2019.106295_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.2465/jmps.180716_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2014.01.033_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"},{"@type":"CROSSREF","@value":"10.1016/j.jseaes.2016.12.033_references_DOI_18I1iAPRDFASHwHn54xTio9xTbO"}]}