{"@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/1360855569737267968.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2007gl031718"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2007GL031718"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2007GL031718"}}],"dc:title":[{"@value":"Aluminous hydrous mineral <i>δ</i>‐AlOOH as a carrier of hydrogen into the core‐mantle boundary"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>In‐situ X‐ray diffraction experiments were conducted to determine the stability field of the aluminous hydrous mineral <jats:italic>δ</jats:italic>‐AlOOH over the entire conditions of the lower mantle. We observed <jats:italic>δ</jats:italic>‐AlOOH at pressures from 33 to 134 GPa at 1350–2300 K, indicating that this hydrous mineral in the sediment layer of a subducting slab could transport hydrogen into the core‐mantle boundary (CMB).</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380855569737267975","@type":"Researcher","foaf:name":[{"@value":"Asami Sano"}],"jpcoar:affiliationName":[{"@value":"Institute of Mineralogy, Petrology and Economic Geology, Faculty of Science Tohoku University  Sendai Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380855569737267969","@type":"Researcher","foaf:name":[{"@value":"Eiji Ohtani"}],"jpcoar:affiliationName":[{"@value":"Institute of Mineralogy, Petrology and Economic Geology, Faculty of Science Tohoku University  Sendai Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380855569737267974","@type":"Researcher","foaf:name":[{"@value":"Tadashi Kondo"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Space Science, Graduate School of Science Osaka University  Osaka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380855569737267973","@type":"Researcher","foaf:name":[{"@value":"Naohisa Hirao"}],"jpcoar:affiliationName":[{"@value":"Japan Synchrotron Radiation Research Institute  Sayo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380855569737267972","@type":"Researcher","foaf:name":[{"@value":"Takeshi Sakai"}],"jpcoar:affiliationName":[{"@value":"Institute of Mineralogy, Petrology and Economic Geology, Faculty of Science Tohoku University  Sendai Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380855569737267971","@type":"Researcher","foaf:name":[{"@value":"Nagayoshi Sata"}],"jpcoar:affiliationName":[{"@value":"Japan Marine Science and Technology Center Japan Agency for Marine‐Earth Science and Technology  Yokosuka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380855569737267968","@type":"Researcher","foaf:name":[{"@value":"Yasuo Ohishi"}],"jpcoar:affiliationName":[{"@value":"Japan Synchrotron Radiation Research Institute  Sayo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380855569737267970","@type":"Researcher","foaf:name":[{"@value":"Takumi Kikegawa"}],"jpcoar:affiliationName":[{"@value":"Photon Factory High Energy Accelerator Research Organization  Tsukuba Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2008-02","prism:volume":"35","prism:number":"3","prism:startingPage":"L03303"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2007GL031718"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2007GL031718"}],"createdAt":"2008-02-01","modifiedAt":"2023-10-31","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050287540562306176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spin Transition of Iron in δ‐(Al,Fe)OOH Induces Thermal Anomalies in Earth's Lower Mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1050850412716474624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Compressional behavior and spin state of δ-(Al,Fe)OOH at high pressures"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215916234368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Symmetrization driven spin transition in ε-FeOOH at high pressure"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215916266624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stability of a hydrous δ-phase, AlOOH–MgSiO2(OH)2, and a mechanism for water transport into the base of lower mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216799523968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The pyrite-type high-pressure form of FeOOH"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229844621440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stability of Hydrous Minerals and Water Reservoirs in the Deep Earth Interior"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004231198553728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Compression behaviors of distorted rutile-type hydrous phases, MOOH (M = Ga, In, Cr) and CrOOD"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004231198659712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Observation of pressure-induced phase transition of δ-AlOOH by using single-crystal synchrotron X-ray diffraction method"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233489147776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Direct observation of symmetrization of hydrogen bond in δ-AlOOH under mantle conditions using neutron diffraction"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005516841542400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stability of Fe-bearing hydrous phases and element partitioning in the system MgO–Al2O3–Fe2O3–SiO2–H2O in Earth's lowermost mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142866869376","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Chemical Reaction Between Metallic Iron and a Limited Water Supply Under Pressure: Implications for Water Behavior at the Core‐Mantle Boundary"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168779014400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The influence of δ-(Al,Fe)OOH on seismic heterogeneities in Earth’s lower mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168779097600","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Phase transitions of ScOOH under high pressure"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021390563132288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Hydrogen partitioning between stishovite and hydrous phase δ: implications for water cycle and distribution in the lower mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283690266665088","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High-pressure X-ray diffraction study of ε-FeOOH"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285706175541120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermal equation of state of MgSiO4H2 phase H determined by in situ X-ray diffraction and a multianvil apparatus"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707150737920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Conjecture with water and rheological control for subducting slab in the mantle transition zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360286991877813376","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"New aluminium hydroxide at multimegabar pressures: Implications for water reservoirs in deep planetary interiors"}]},{"@id":"https://cir.nii.ac.jp/crid/1360286993150120960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Solid Solution and Compression Behavior of Hydroxides in the Lower Mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617879594112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Structural Study of δ-AlOOH Up to 29 GPa"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643730426752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Al partitioning between phase D and bridgmanite at the uppermost lower mantle pressure"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643803116032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The role of water in Earth's mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165811086080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Hydrous minerals and the storage of water in the deep mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166067185536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stability of Fe–Ni hydride after the reaction between Fe–Ni alloy and hydrous phase (δ-AlOOH) up to 1.2Mbar: Possibility of H contribution to the core density deficit"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166760641152","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stability of hydrous silicate at high pressures and water transport to the deep lower mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179757907328","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sound velocities of δ‐AlOOH up to core‐mantle boundary pressures with implications for the seismic anomalies in the deep mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179761845120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Elasticity of <i>ε</i>‐FeOOH: Seismic implications for Earth's lower mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092695162496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Elastic Properties of the Pyrite‐Type FeOOH‐AlOOH System From First‐Principles Calculations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092854380416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Melting phase relation of Fe-bearing Phase D up to the uppermost lower mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576215428173824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Aluminum and hydrogen partitioning between bridgmanite and high-pressure hydrous phases: Implications for water storage in the lower mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580232405401344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Calculated Elasticity of Al-Bearing Phase D"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654738132992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Chemical Reactions Between Fe and H<sub>2</sub>O up to Megabar Pressures and Implications for Water Storage in the Earth's Mantle and Core"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848656128664960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effects of Mg and Si ions on the symmetry of δ-AlOOH"}]},{"@id":"https://cir.nii.ac.jp/crid/1360849946243345536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ab Initio Study on the Lower Mantle Minerals"}]},{"@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/1360865815498567680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Equation of State and Spin Crossover of (Al, Fe)‐Phase H"}]},{"@id":"https://cir.nii.ac.jp/crid/1363946392956783872","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Solubility behavior of δ-AlOOH and ε-FeOOH at high pressures"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206544682496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Stability field of phase Egg, AlSiO<sub>3</sub>OH at high pressure and high temperature: possible water reservoir in mantle transition zone"},{"@value":"Stability field of phase Egg, AlSiO3OH at high pressure and high temperature: possible water reservoir in mantle transition zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206545503104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Pressure–volume–temperature equation of state of ε–FeOOH to 11 GPa and 700 K"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679065235968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"第一原理電子状態計算法を用いた地球深部における含水鉱物の構造・物性研究"},{"@language":"en","@value":"First Principles Investigations of the Hydrous Minerals in the Earth's Deep Interior"},{"@language":"ja-Kana","@value":"ダイイチ ゲンリ デンシ ジョウタイ ケイサンホウ オ モチイタ チキュウ シンブ ニ オケル ガンスイ コウブツ ノ コウゾウ ・ ブッセイ ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679357216256","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Neutron Scattering Experiments at High Pressure - Experiences in ISIS"},{"@language":"ja","@value":"ＩＳＩＳ　における高圧下中性子散乱実験の実際"},{"@language":"ja-Kana","@value":"ISIS ニ オケル コウアツカ チュウセイシ サンラン ジッケン ノ ジッサイ"},{"@value":"Neutron Scattering Experiments at High Pressure — Experiences in ISIS"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679358736128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"地球惑星内部における含水物質の理論的研究"},{"@language":"en","@value":"Computational Investigation on the Hydrous Material in the Earth and Planetary Interiors"},{"@language":"ja-Kana","@value":"チキュウ ワクセイ ナイブ ニ オケル ガンスイ ブッシツ ノ リロンテキ ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681522882944","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"X-ray diffraction study of high pressure transition in InOOH"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681523587328","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Compression behavior of manganite"}]},{"@id":"https://cir.nii.ac.jp/crid/1390292118448998784","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"In situ X–ray diffraction study of the phase boundary between diaspore and δ–AlOOH"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238044644224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"中性子散乱実験により明らかにする鉱物中の水素結合とその役割"},{"@language":"en","@value":"Neutron Diffraction Study on Hydrogen Bond in Mineral in the Deep Earth"},{"@value":"受賞記事 中性子散乱実験により明らかにする鉱物中の水素結合とその役割"},{"@language":"ja-Kana","@value":"ジュショウ キジ チュウセイシ サンラン ジッケン ニ ヨリ アキラカ ニ スル コウブツ チュウ ノ スイソ ケツゴウ ト ソノ ヤクワリ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390845713082351616","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Sound velocity measurements of ε–FeOOH up to 24 GPa"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367089653888","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The role of hydrogen bonds in hydrous minerals stable at lower mantle pressure conditions"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2007gl031718"},{"@type":"OPENAIRE","@value":"doi_dedup___::4a3170982edfce822533d9e7e6cc371b"},{"@type":"CROSSREF","@value":"10.1038/nature22823_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1002/9781118992487.ch21_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1007/s00269-012-0487-y_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1007/s00269-013-0649-6_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1038/s41598-018-33598-2_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.2138/am-2019-6913_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.5940/jcrsj.60.48_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1029/2020gl089616_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.5611/hamon.22.2_162_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1038/s41598-021-91180-9_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1080/08957959.2021.1964495_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1186/s40645-022-00521-3_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.2465/jmps.160719e_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1186/s40645-024-00615-0_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1007/s00269-009-0319-x_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1007/s00269-018-0980-z_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1029/2019jb018146_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.2465/jmps.071022m_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.2465/jmps.130621b_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.3390/min10121055_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1007/s00269-021-01163-5_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1093/nsr/nwz071_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.2465/jmps.211215_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1038/ngeo2074_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1002/2015jb012477_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1002/2017jb014168_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2014.05.059_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1016/j.icarus.2019.113539_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1029/2021gc009703_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2022.117441_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.3390/min12080922_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1002/2017gl075720_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1007/s00269-011-0445-0_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.2465/jmps.160719c_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1146/annurev-earth-071719-055139_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1016/j.chemgeo.2015.05.005_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.4131/jshpreview.19.31_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1029/2020gl087036_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.2138/am-2021-7605_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.2138/am-2021-7907_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1029/2022jb026291_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2013.08.012_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.2465/jmps.181115b_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.4131/jshpreview.27.183_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1016/j.gsf.2013.12.005_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2012.01.002_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.2138/am-2019-7064_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2019.115714_references_DOI_C1NBZAhazKcQd9s3zhAx7nojgwo"}]}