{"@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/1360004229806369280.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2016jb013091"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016JB013091"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2016JB013091"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2016JB013091"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/am-pdf/10.1002/2016JB013091"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016JB013091"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Along‐arc variation in short‐term slow slip events caused by 3‐D fluid migration in subduction zones"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>A strong correlation exists between the average slip rate by short‐term slow slip events (SSEs) and changes in the slab geometry in Cascadia and Nankai. The generation of short‐term SSEs is generally assumed to be related to the presence of fluids and we investigate the hypothesis that fluids released by metamorphic dehydration reactions migrate in 3‐D due to complex slab geometry. The associated along‐arc focusing of fluid flux is likely to cause higher average slip rate in certain patches. To test this hypothesis, we investigate how fluid migration is modified by along‐strike changes in slab geometry. We use a numerical model of two‐phase flow in subduction zones. In this model fluids migrate subparallel to the slab surface due to the anisotropic permeability inside a serpentinite layer just above the slab. In 3‐D, we find that fluids migrate in the maximum‐dip direction of the slab, rather than subparallel to the plate motion. As a result fluid paths concentrate with increasing porosity where the slab has a convex shape (and diverge with decreasing porosity where it has a concave shape). These results suggest that regions with a high average slip rate by short‐term SSEs in Cascadia and Nankai can be explained by 3‐D focusing of fluid migration. We predict a defocusing of fluids below the Kii Channel, Nankai, which may be the reason for the observed small slip by short‐term SSEs in this location.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004229806368900","@type":"Researcher","foaf:name":[{"@value":"M. Morishige"}],"jpcoar:affiliationName":[{"@value":"Institute for Geothermal Sciences, Graduate School of Science Kyoto University  Beppu Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229806369415","@type":"Researcher","foaf:name":[{"@value":"Peter E. van Keken"}],"jpcoar:affiliationName":[{"@value":"Department of Terrestrial Magnetism Carnegie Institution for Science  Washington District of Columbia USA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"21699313"},{"@type":"EISSN","@value":"21699356"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2017-02","prism:volume":"122","prism:number":"2","prism:startingPage":"1434","prism:endingPage":"1448"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#am","http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016JB013091"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2016JB013091"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2016JB013091"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/am-pdf/10.1002/2016JB013091"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016JB013091"}],"createdAt":"2017-01-20","modifiedAt":"2023-10-04","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781902869376","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16H06477"},{"@type":"JGN","@value":"JP16H06477"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-16H06477/"}],"notation":[{"@language":"ja","@value":"低速変形から高速すべりまでの地球科学的モデル構築"},{"@language":"en","@value":"Study on Geoscientific Modeling of Earthquake Phenomena from Low-speed Deformation to High-speed Slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282256900963328","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16K17792"},{"@type":"JGN","@value":"JP16K17792"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-16K17792/"}],"notation":[{"@language":"ja","@value":"流体の3次元的移動の観点に基づくスロー地震の仕組みの解明"},{"@language":"en","@value":"Understanding of the mechanisms of slow earthquakes in terms of 3D fluid migration"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202746187904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional seismic velocity structure and configuration of the Philippine Sea slab in southwestern Japan estimated by double-difference tomography"}]},{"@id":"https://cir.nii.ac.jp/crid/1050282677748874240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Subduction of the Philippine Sea plate beneath southwestern Japan: Slab geometry and its relationship to arc magmatism"}]},{"@id":"https://cir.nii.ac.jp/crid/1050859215942088064","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Along-strike distribution of seismicity and large slow slip correlated with gravity at the Nankai Trough"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229801701248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"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/1360004229807600000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Fluid Migration in a Subducting Viscoelastic Slab"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004230122187520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Shear‐induced permeability anisotropy of simulated serpentinite gouge produced by triaxial deformation experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011143890043776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Generation and Compaction of Partially Molten Rock"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144270517376","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Weakening of the slab–mantle wedge interface induced by metasomatic growth of talc"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144436945408","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An inverted continental Moho and serpentinization of the forearc mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145105475968","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"High-Pressure Creep of Serpentine, Interseismic Deformation, and Initiation of Subduction"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617909532032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"New, improved version of generic mapping tools released"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617909770624","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Nonvolcanic Deep Tremor Associated with Subduction in Southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617915364736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A model for the global variation in oceanic depth and heat flow with lithospheric age"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621162676096","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Effect of three‐dimensional slab geometry on deformation in the mantle wedge: Implications for shear wave anisotropy"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166661644928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Split Philippine Sea plate beneath Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166662193792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional structure of P-wave anisotropy in the presence of small-scale convection in the mantle wedge"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565168428158336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Permeability anisotropy of serpentinite and fluid pathways in a subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182088843904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"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/1360567183389966720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Episodic tremor and slow slip potentially linked to permeability contrasts at the Moho"}]},{"@id":"https://cir.nii.ac.jp/crid/1360568693236262144","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Crystallographic preferred orientation of talc determined by an improved EBSD procedure for sheet silicates: Implications for anisotropy at the slab–mantle interface due to Si-metasomatism"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092884419328","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Episodic slow slip events accompanied by non‐volcanic tremors in southwest Japan subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092886258944","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Low-frequency earthquakes in Shikoku, Japan, and their relationship to episodic tremor and slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574093445368064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Anisotropic structures of oceanic slab and mantle wedge in a deep low‐frequency tremor zone beneath the Kii Peninsula, SW Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094117075456","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Flow in deformable porous media. Part 2 Numerical analysis – the relationship between shock waves and solitary waves"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095818154496","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A two‐phase model for compaction and damage: 1. General Theory"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567866151424","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Simple 2-D models for melt extraction at mid-ocean ridges and island arcs"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869855136952320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Fault‐Valve Instability: A Mechanism for Slow Slip Events"}]},{"@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/1361137043407333120","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A community benchmark for subduction zone modeling"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137044763238016","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Weakening of the subduction interface and its effects on surface heat flow, slab dehydration, and mantle wedge serpentinization"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045659518464","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Stability and dynamics of serpentinite layer in subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518777935488","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Thermal structure beneath Tohoku, northeast japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519121173120","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Age, spreading rates, and spreading asymmetry of the world's ocean crust"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520255508224","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mantle flow and deformation of subducting slab at a plate junction"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520816939136","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Finite Element Methods and Navier-Stokes Equations"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520940507776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Slow Earthquakes and Nonvolcanic Tremor"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418521296042496","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seismic Consequences of Warm Versus Cool Subduction Metamorphism: Examples from Southwest and Northeast Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995792649856","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Source parameters and time‐dependent slip distributions of slow slip events on the Cascadia subduction zone from 1998 to 2008"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468389109248","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Low‐frequency tremors, intraslab and interplate earthquakes in Southwest Japan—from a viewpoint of slab dehydration"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981469036268032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"H<sub>2</sub>O subduction beyond arcs"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470741360768","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Non-volcanic tremor and low-frequency earthquake swarms"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981471310349184","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Depth of seismic coupling along subduction zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544418900404096","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The slip distribution of the 1946 Nankai earthquake estimated from tsunami inversion using a new plate model"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420329762688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Detection of short‐term slow slip events along the Nankai Trough, southwest Japan, using GNSS data"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544421132538880","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rheology of the Upper Mantle: A Synthesis"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893373320576","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Subduction factory: 4. Depth-dependent flux of H<sub>2</sub>O from subducting slabs worldwide"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894317670272","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Subduction zone anisotropy beneath Corvallis, Oregon: A serpentinite skid mark of trench‐parallel terrane migration?"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825896404139776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Characteristics and interactions between non-volcanic tremor and related slow earthquakes in the Nankai subduction zone, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369922408064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Magma migration and magmatic solitary waves in 3‐D"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370470459392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mechanics of Fluid-Rock Systems"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370556176256","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The instantaneous rotation vector of the Philippine sea plate relative to the Eurasian plate"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370961661440","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Fluid flow in subduction zones: The role of solid rheology and compaction pressure"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844187840000","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Flow in deformable porous media. Part 1 Simple analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844242379392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Episodic Tremor and Slip on the Cascadia Subduction Zone: The Chatter of Silent Slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318762296704","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"High‐resolution models of subduction zones: Implications for mineral dehydration reactions and the transport of water into the deep mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794386719360","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A new regime of slab-mantle coupling at the plate interface and its possible implications for the distribution of volcanoes"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794865241216","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Finite deformation during fluid flow"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269991901952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Slow Earthquakes Coincident with Episodic Tremors and Slow Slip Events"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270426238080","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Silent Slip Event on the Deeper Cascadia Subduction Interface"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270893240320","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Numerical simulation of geodynamic processes with the Portable Extensible Toolkit for Scientific Computation"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270939751168","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Melt-preferred orientation, anisotropic permeability and melt-band formation in a deforming, partially molten aggregate"}]},{"@id":"https://cir.nii.ac.jp/crid/1370569767715513984","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Depth to the Juan de Fuca Slab Beneath the Cascadia Subduction Margin – A 3‐D Model for Sorting Earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681487030784","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Evolution of the Shikoku Basin."}]},{"@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/2050307417163364224","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A long-term slow slip event from 1996 to 1997 in the Kii Channel, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317073908352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Can clay minerals account for the behavior of non-asperity on the subducting plate interface？"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1002/2016jb013091"},{"@type":"KAKEN","@value":"PRODUCT-21626147"},{"@type":"KAKEN","@value":"PRODUCT-21307091"},{"@type":"OPENAIRE","@value":"doi_dedup___::b930e864397039e342c17899f2d277a1"},{"@type":"CROSSREF","@value":"10.1002/2017gc007236_references_DOI_RqWuFIu7902T94uxAcXGaN4H600"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2022.117824_references_DOI_RqWuFIu7902T94uxAcXGaN4H600"},{"@type":"CROSSREF","@value":"10.2138/am-2020-7006_references_DOI_RqWuFIu7902T94uxAcXGaN4H600"},{"@type":"CROSSREF","@value":"10.1029/2024jb029165_references_DOI_9Oq3arngCaQdp7wFoZ68uVPaZQC"},{"@type":"CROSSREF","@value":"10.1029/2018jb017068_references_DOI_RqWuFIu7902T94uxAcXGaN4H600"},{"@type":"CROSSREF","@value":"10.4294/zisin.2017-10_references_DOI_RqWuFIu7902T94uxAcXGaN4H600"}]}