{"@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/1361699995676677376.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.1087132"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.1087132"}}],"dc:title":[{"@value":"Melt Segregation and Strain Partitioning: Implications for Seismic Anisotropy and Mantle Flow"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>\n            One of the principal means of understanding upper mantle dynamics involves inferring mantle flow directions from seismic anisotropy under the assumption that the seismic fast direction (olivine\n            <jats:italic>a</jats:italic>\n            axis) parallels the regional flow direction. We demonstrate that (i) the presence of melt weakens the alignment of\n            <jats:italic>a</jats:italic>\n            axes and (ii) when melt segregates and forms networks of weak shear zones, strain partitions between weak and strong zones, resulting in an alignment of\n            <jats:italic>a</jats:italic>\n            axes 90° from the shear direction in three-dimensional deformation. This orientation of\n            <jats:italic>a</jats:italic>\n            axes provides a new means of interpreting mantle flow from seismic anisotropy in partially molten deforming regions of Earth.\n          </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380017280655046278","@type":"Researcher","foaf:name":[{"@value":"B. K. Holtzman"}],"jpcoar:affiliationName":[{"@value":"Department of Geology and Geophysics, University of Minnesota, Minneapolis, MN 55455, USA. Bayerisches Geoinstitut, Bayreuth, D-95440, Germany."}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995676677377","@type":"Researcher","foaf:name":[{"@value":"D. L. Kohlstedt"}],"jpcoar:affiliationName":[{"@value":"Department of Geology and Geophysics, University of Minnesota, Minneapolis, MN 55455, USA. Bayerisches Geoinstitut, Bayreuth, D-95440, Germany."}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995676677376","@type":"Researcher","foaf:name":[{"@value":"M. E. Zimmerman"}],"jpcoar:affiliationName":[{"@value":"Department of Geology and Geophysics, University of Minnesota, Minneapolis, MN 55455, USA. Bayerisches Geoinstitut, Bayreuth, D-95440, Germany."}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995676677378","@type":"Researcher","foaf:name":[{"@value":"F. Heidelbach"}],"jpcoar:affiliationName":[{"@value":"Department of Geology and Geophysics, University of Minnesota, Minneapolis, MN 55455, USA. Bayerisches Geoinstitut, Bayreuth, D-95440, Germany."}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995676677381","@type":"Researcher","foaf:name":[{"@value":"T. Hiraga"}],"jpcoar:affiliationName":[{"@value":"Department of Geology and Geophysics, University of Minnesota, Minneapolis, MN 55455, USA. Bayerisches Geoinstitut, Bayreuth, D-95440, Germany."}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995676677379","@type":"Researcher","foaf:name":[{"@value":"J. Hustoft"}],"jpcoar:affiliationName":[{"@value":"Department of Geology and Geophysics, University of Minnesota, Minneapolis, MN 55455, USA. Bayerisches Geoinstitut, Bayreuth, D-95440, Germany."}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00368075"},{"@type":"EISSN","@value":"10959203"}],"prism:publicationName":[{"@value":"Science"}],"dc:publisher":[{"@value":"American Association for the Advancement of Science (AAAS)"}],"prism:publicationDate":"2003-08-29","prism:volume":"301","prism:number":"5637","prism:startingPage":"1227","prism:endingPage":"1230"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.1087132"}],"createdAt":"2003-08-28","modifiedAt":"2024-01-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001338868540416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Direct evidence for upper mantle structure in the NW Pacific Plate : Microstructural analysis of a petit-spot peridotite xenolith"},{"@value":"Direct evidence for upper mantle structure within the NW Pacific Plate: microstructural analyses of a petit-spot peridotite xenolith"}]},{"@id":"https://cir.nii.ac.jp/crid/1050564288821961472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Spatial variations in antigorite fabric across a serpentinite subduction channel : Insights from the Ohmachi Seamount, Izu-Bonin frontal arc"},{"@value":"Spatial variations in antigorite fabric across a serpentinite subduction channel: insights from the Ohmachi Seamount, Izu-Bonin arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1050845763798672128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Rheological contrast between garnet and clinopyroxene in the mantle wedge : An example from Higashi-akaishi peridotite mass, SW Japan"},{"@value":"Rheological contrast between garnet and clinopyroxene in the mantle wedge: an example from Higashi-akaishi peridotite mass"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232135126912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Well-wetted olivine grain boundaries in partially molten peridotite in the asthenosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232135378560","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electrical conductivity anisotropy in partially molten peridotite under shear deformation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025429411606656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Deformation and melt–rock interaction in the upper mantle: Insights from the layered structure of the Horoman peridotite, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025431120536320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Structural evolution of the Horoman peridotite complex in conjunction with the formation of the Hidaka Metamorphic Belt, Hokkaido"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283690892886144","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismic anisotropy of the uppermost mantle beneath the Rio Grande rift: Evidence from Kilbourne Hole peridotite xenoliths, New Mexico"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707112174464","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Natural olivine crystal-fabrics in the western Pacific convergence region: A new method to identify fabric type"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707402318592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Estimating the electrical conductivity of the melt phase of a partially molten asthenosphere from seafloor magnetotelluric sounding data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285710774738944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Petrological, petrofabric, and oxygen isotopic study of five ungrouped meteorites related to brachinites"}]},{"@id":"https://cir.nii.ac.jp/crid/1360286991818272640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Temperature-enhanced electrical conductivity anisotropy in partially molten peridotite under shear deformation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617556400128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rheology of the Fluid Oversaturated Fault Zones at the Brittle‐Plastic Transition"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306905179136000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Textural and chemical variations in peridotite induced by hydrous melt migration in mantle under the back-arc spreading"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565164304089216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Varying deformation patterns in central Tibet revealed by radial anisotropy tomography"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166662998656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Subduction of oceanic asthenosphere: Evidence from sub‐slab seismic anisotropy"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179757086976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Density and seismic velocity of hydrous melts under crustal and upper mantle conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567181152202368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Deformation history of Pinatubo peridotite xenoliths: constraints from microstructural observation and determination of olivine slip systems"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567181183852672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Transport properties of olivine grain boundaries from electrical conductivity experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182088881280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Temperature dependence of [100](010) and [001](010) dislocation mobility in natural olivine"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182379047936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"In situ observation of crystallographic preferred orientation of deforming olivine at high pressure and high temperature"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118713913600","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Enhancement of ductile deformation in polycrystalline anorthite due to the addition of water"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580232380407168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mantle deformation during opening of the Japan Sea back-arc: Insights from peridotite xenoliths, Kawashimo, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584339775252736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Variation in olivine crystal-fabrics and their seismic anisotropies in the Horoman peridotite complex, Hokkaido, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846639279022336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"<i>P</i> wave radial anisotropy tomography of the upper mantle beneath the North China Craton"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657065428992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Subduction of oceanic asthenosphere: A critical appraisal in central Alaska"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657065468288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dehydration breakdown of antigorite and the formation of B-type olivine CPO"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657932196992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Consequences of viscous anisotropy in a deforming, two-phase aggregate. Part 1. Governing equations and linearized analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848658349913216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Olivine crystals align during diffusion creep of Earth’s upper mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848661227085696","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismic and Electrical Signatures of the Lithosphere–Asthenosphere System of the Normal Oceanic Mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567420619776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Upper mantle seismic anisotropy beneath the Northern Transantarctic Mountains inferred from peridotite xenoliths near Mt. Melbourne, northern Victoria Land, Antarctica"}]},{"@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/1360857593697433472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Limited impact of anisotropic thermal conductivity in the mantle wedge on the slab temperature in the Tohoku subduction zone, Northeast Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593710824064","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Deformation beneath Gakkel Ridge, Arctic Ocean: From mantle flow to mantle shear in a sparsely magmatic spreading zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861705562126592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Anisotropic Tomography and Dynamics of the Big Mantle Wedge"}]},{"@id":"https://cir.nii.ac.jp/crid/1361694368212654848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Melting of recycled ancient crust responsible for the Gutenberg discontinuity"}]},{"@id":"https://cir.nii.ac.jp/crid/1361975287127806336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermoelastic properties of ice VII and its high-pressure polymorphs: Implications for dynamics of cold slab subduction in the lower mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204229983616","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Structure Sensitivity and Elastic Anisotropy within Peridotites"},{"@language":"ja","@value":"かんらん岩の構造敏感性と弾性的異方性"},{"@language":"ja-Kana","@value":"カンランガン ノ コウゾウ ビンカンセイ ト ダンセイテキ イホウセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303000832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Anisotropic Velocity Structure of Seismic Waves in Japan Subduction Zone"},{"@language":"ja","@value":"日本列島の地震波異方性速度構造"},{"@language":"ja-Kana","@value":"ニホン レットウ ノ ジシンハ イホウセイ ソクド コウゾウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206526238464","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Olivine fabrics: a key to explore upper mantle structure"},{"@value":"かんらん石ファブリック：上部マントル構造を探る手がかり"},{"@language":"ja-Kana","@value":"カンランセキ ファブリック : ジョウブ マントル コウゾウ オ サグル テガカリ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206526524672","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seismic anisotropy in subduction zones and lattice-preferred orientation of olivine"},{"@language":"ja","@value":"沈み込み帯での地震波異方性とかんらん石の格子選択配向"},{"@value":"日本鉱物科学会研究奨励賞第3回受賞者 受賞記念研究紹介 沈み込み帯での地震波異方性とかんらん石の格子選択配向"},{"@language":"ja-Kana","@value":"ニホン コウブツ カガクカイ ケンキュウ ショウレイショウ ダイ3カイ ジュショウシャ ジュショウ キネン ケンキュウ ショウカイ シズミ コミ タイ デ ノ ジシンハ イホウセイ ト カンランセキ ノ コウシ センタクハイコウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390025197284350976","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"幌満かんらん岩体の変形構造：構造岩石学的研究の現状と新展開"},{"@language":"en","@value":"Deformation structure of the Horoman peridotite complex: Overview of microstructural and petrological variation and beyond"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679213864576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"蛇紋岩の力学的性質とそのテクトニックな意義"},{"@language":"en","@value":"Rheological Properties of Serpentinite and Their Tectonic Significance"},{"@language":"ja-Kana","@value":"ジャモンガン ノ リキガクテキ セイシツ ト ソノ テクトニック ナ イギ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679279748096","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seismic Velocity and Electrical Conductivity of Rocks in the Crust and Mantle: Probing Water in Subduction Zones"},{"@language":"ja","@value":"地殻・マントル物質の地震波速度と電気伝導度：沈み込み帯の水を探る"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680069883392","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"かんらん岩の構造解析と最上部マントルのレオロジー"},{"@language":"en","@value":"Structural Geology of Peridotite and Rheology of the Uppermost Mantle"},{"@language":"ja-Kana","@value":"カンランガン ノ コウゾウ カイセキ ト サイ ジョウブ マントル ノ レオロジー"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681502165888","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Experimental studies on crystallographic preferred orientation of olivine: A review"},{"@language":"ja","@value":"カンラン石の結晶方位定向配列に関する実験的研究：レビュー"},{"@language":"ja-Kana","@value":"カンランセキ ノ ケッショウ ホウイ テイコウ ハイレツ ニ カンスル ジッケンテキ ケンキュウ : レビュー"}]},{"@id":"https://cir.nii.ac.jp/crid/1390870529360675456","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"脆性–塑性遷移領域における岩石の変形と水の効果について"},{"@language":"en","@value":"Effects of Water on the Deformation of Rocks at the Brittle–Plastic Transition: Insight from High-pressure and High-temperature Deformation Experiment on Quartz + Water Aggregates"},{"@value":"脆性-塑性遷移領域における岩石の変形と水の効果について : 石英多結晶体の高含水変形実験からの知見"},{"@language":"ja-Kana","@value":"ゼイセイ-ソセイ センイ リョウイキ ニ オケル ガンセキ ノ ヘンケイ ト ミズ ノ コウカ ニ ツイテ : セキエイ タケッショウタイ ノ コウガンスイ ヘンケイ ジッケン カラ ノ チケン"}]},{"@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"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1126/science.1087132"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2010.09.037_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2013.02.010_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2011.09.013_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2013.11.025_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1186/s40645-022-00476-5_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2024.230508_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2025.0039_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2024.230535_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1111/maps.13249_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2016.02.029_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.2465/gkk.39.12_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.4294/zisin.61.187_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.2465/gkk.120712b_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2010.12.011_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2013.12.004_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1029/2020jb020804_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.lithos.2024.107776_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1002/2016jb012832_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1029/2012gl052639_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1002/2015gc006242_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1007/s00269-016-0853-2_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1007/s00410-018-1468-z_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2010.08.035_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2010.10.008_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.jsg.2022.104547_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2023.229722_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.jog.2023.102006_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1002/2014gc005279_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1017/jfm.2013.482_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1038/nature12570_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2014.08.018_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.5026/jgeography.124.371_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.5026/jgeography.117.93_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.2465/gkk.120828_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.4294/zisin.61.541_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2019.115922_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.jsg.2020.104237_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.gsf.2021.101342_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2021.229110_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2021.229186_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1029/2021gl097550_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.5026/jgeography.135.33_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2009.04.007_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2015.04.004_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1038/s41467-019-13958-w_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1146/annurev-earth-063016-020319_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1678/rheology.34.291_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2016.03.019_references_DOI_3iDeeY4fgefMpJQy1ceE6zPSnqC"}]}