{"@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/1363388846269680256.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2003jb002562"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2003JB002562"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2003JB002562"}},{"identifier":{"@type":"HANDLE","@value":"20.500.11820/744bdb9f-83cc-4e25-a662-5f8c434d304d"}},{"identifier":{"@type":"HANDLE","@value":"1983/a3ab2b00-ddf6-43ca-a2b8-5723df952f84"}}],"dc:title":[{"@value":"Experimentally determined postspinel transformation boundary in Mg<sub>2</sub>SiO<sub>4</sub> using MgO as an internal pressure standard and its geophysical implications"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We have determined the postspinel transformation boundary in Mg<jats:sub>2</jats:sub>SiO<jats:sub>4</jats:sub> by combining quench technique with in situ pressure measurements, using multiple internal pressure standards including Au, MgO, and Pt. The experimentally determined boundary is in general agreement with previous in situ measurements in which the Au scale of <jats:ext-link xmlns:xlink=\"http://www.w3.org/1999/xlink\" xlink:href=\"#jgrb13858-bib-0001\"><jats:italic>Anderson et al.</jats:italic> [1989]</jats:ext-link> was used to calculate pressure: Using this pressure scale, it occurs at significantly lower pressures compared to that corresponding to the 660‐km seismic discontinuity. In this study, we also report new experimental data on the transformation boundary determined using MgO as an internal standard. The results show that the transition boundary is located at pressures close to the 660‐km discontinuity using the MgO pressure scale of <jats:ext-link xmlns:xlink=\"http://www.w3.org/1999/xlink\" xlink:href=\"#jgrb13858-bib-0020\"><jats:italic>Speziale et al.</jats:italic> [2001]</jats:ext-link> and can be represented by a linear equation, <jats:italic>P</jats:italic>(GPa) = 25.12 − 0.0013<jats:italic>T</jats:italic>(°C). The Clapeyron slope for the postspinel transition boundary is precisely determined and is significantly less negative than previous estimates. Our results, based on the MgO pressure scale, support the conventional hypothesis that the postspinel transformation is responsible for the observed 660‐km seismic discontinuity.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004231198815104","@type":"Researcher","foaf:name":[{"@value":"Y. Fei"}],"jpcoar:affiliationName":[{"@value":"Geophysical Laboratory Carnegie Institution of Washington  Washington DC USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846269680256","@type":"Researcher","foaf:name":[{"@value":"J. Van Orman"}],"jpcoar:affiliationName":[{"@value":"Geophysical Laboratory Carnegie Institution of Washington  Washington DC USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846269680258","@type":"Researcher","foaf:name":[{"@value":"J. Li"}],"jpcoar:affiliationName":[{"@value":"Geophysical Laboratory Carnegie Institution of Washington  Washington DC USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846269680259","@type":"Researcher","foaf:name":[{"@value":"W. van Westrenen"}],"jpcoar:affiliationName":[{"@value":"Geophysical Laboratory Carnegie Institution of Washington  Washington DC USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846269680257","@type":"Researcher","foaf:name":[{"@value":"C. Sanloup"}],"jpcoar:affiliationName":[{"@value":"Geophysical Laboratory Carnegie Institution of Washington  Washington DC USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846269680262","@type":"Researcher","foaf:name":[{"@value":"W. Minarik"}],"jpcoar:affiliationName":[{"@value":"Geophysical Laboratory Carnegie Institution of Washington  Washington DC USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846269680264","@type":"Researcher","foaf:name":[{"@value":"K. Hirose"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Sciences Tokyo Institute of Technology  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846269680260","@type":"Researcher","foaf:name":[{"@value":"T. Komabayashi"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Sciences Tokyo Institute of Technology  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846269680384","@type":"Researcher","foaf:name":[{"@value":"M. Walter"}],"jpcoar:affiliationName":[{"@value":"Institute for Study of the Earth's Interior Okayama University  Misasa Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846269680261","@type":"Researcher","foaf:name":[{"@value":"K. Funakoshi"}],"jpcoar:affiliationName":[{"@value":"Japan Synchrotron Radiation Research Institute, SPring‐8  Hyogo Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2004-02","prism:volume":"109","prism:number":"B2","prism:startingPage":"B02305"},"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%2F2003JB002562"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2003JB002562"}],"createdAt":"2004-02-06","modifiedAt":"2023-10-12","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002214348529024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Subducted slabs stagnant above, penetrating through, and trapped below the 660 km discontinuity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216113765632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geophysical and mineralogical constraints on the post-spinel transformation for the Tonga slab"}]},{"@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/1360004231198814848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The stability of anhydrous phase B, Mg14Si5O24, at mantle transition zone conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004231906435840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mineralogy of the Deep Mantle – The Post-Perovskite Phase and its Geophysical Significance"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232135200384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Metastable olivine wedge and deep dry cold slab beneath southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232425602688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High-pressure transitions in NaZnF3 and NaMnF3 perovskites, and crystal-chemical characteristics of perovskite–postperovskite transitions in ABX3 fluorides and oxides"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232425659648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Phase relations and mineral chemistry in pyrolitic mantle at 1600–2200 °C under pressures up to the uppermost lower mantle: Phase transitions around the 660-km discontinuity and dynamics of upwelling hot plumes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233285030016","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Basaltic accumulation instability and chaotic plate motion in the earliest mantle inferred from numerical experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004236017782272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Phase Relations in the Model System SiO2–MgO–Cr2O3: Evidence from the Results of Experiments in Petrologically Significant Sections at 12–24 GPa and 1600°C"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005517197823360","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effect of pressure on temperature measurements using WRe thermocouple and its geophysical impact"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017282443923328","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Hadean mantle oxidation inferred from melting of peridotite under lower-mantle conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017282446267392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reassessment of a bond correction method for in situ ultrasonic interferometry on elastic wave velocity measurement under high pressure and high temperature"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021389799116160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Partitioning of Fe2+ and Fe3+ between bridgmanite and silicate melt: Implications for redox evolution of the Earth's mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704778037504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mantle evolution in Venus due to magmatism and phase transitions: From punctuated layered convection to whole‐mantle convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707112220928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mantle transition zone beneath a normal seafloor in the northwestern Pacific: Electrical conductivity, seismic thickness, and water content"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707402309120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sound velocities measurement on MgSiO3 akimotoite at high pressures and high temperatures with simultaneous in situ X-ray diffraction and ultrasonic study"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708268359040","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"New High‐Pressure Forms of Al<sub>2</sub>SiO<sub>5</sub>"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708462529536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Complete agreement of the post-spinel transition with the 660-km seismic discontinuity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166660658048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Unified analyses for <i>P</i>‐<i>V</i>‐<i>T</i> equation of state of MgO: A solution for pressure‐scale problems in high <i>P</i>‐<i>T</i> experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166662499840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"<i>P</i>‐<i>V</i>‐<i>T</i> equation of state of MgSiO<sub>3</sub> perovskite based on the MgO pressure scale: A comprehensive reference for mineralogy of the lower mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179754220928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Two‐stage evolution of the Earth's mantle inferred from numerical simulation of coupled magmatism‐mantle convection system with tectonic plates"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567181152187520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High-pressure high-temperature phase relations in FeTiO3 up to 35 GPa and 1600 °C"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182088642176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Post-spinel transitions in pyrolite and Mg2SiO4 and akimotoite–perovskite transition in MgSiO3: Precise comparison by high-pressure high-temperature experiments with multi-sample cell technique"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567183240098432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effect of pressure on grain‐growth kinetics of ferropericlase to lower mantle conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118707815680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Depressed 660-km discontinuity caused by akimotoite–bridgmanite transition"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846641639212160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The 3D numerical modeling of subduction dynamics: Plate stagnation and segmentation, and crustal advection in the wet mantle transition zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654734561792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Precise measurements of enthalpy of postspinel transition in Mg<sub>2</sub>SiO<sub>4</sub> and application to the phase boundary calculation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848656128888832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stability region of K0.2Na0.8AlSi3O8 hollandite at 22 GPa and 2273 K"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848661227054976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dynamics in the Uppermost Lower Mantle: Insights into the Deep Mantle Water Cycle Based on the Numerical Modeling of Subducted Slabs and Global-Scale Mantle Dynamics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360849943102091648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Phase Relations of Harzburgite and MORB up to the Uppermost Lower Mantle Conditions: Precise Comparison With Pyrolite by Multisample Cell High‐Pressure Experiments With Implication to Dynamics of Subducted Slabs"}]},{"@id":"https://cir.nii.ac.jp/crid/1360849943103506816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effect of Fe<sup>3+</sup> on Phase Relations in the Lower Mantle: Implications for Redox Melting in Stagnant Slabs"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567354796672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"2-D Numerical Simulations on Formation and Descent of Stagnant Slabs: Important Roles of Trench Migration and Its Temporal Change"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865815685548416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Buoyancy of slabs and plumes enhanced by curved post-garnet phase boundary"}]},{"@id":"https://cir.nii.ac.jp/crid/1361412893239685376","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sharp 660-km discontinuity controlled by extremely narrow binary post-spinel transition"}]},{"@id":"https://cir.nii.ac.jp/crid/1361694368032244992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Three‐Dimensional <i>S</i> Velocity Structure of the Mantle Transition Zone Beneath Central America and the Gulf of Mexico Inferred Using Waveform Inversion"}]},{"@id":"https://cir.nii.ac.jp/crid/1363664919016701056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High-Pressure and High-Temperature Phase Transitions in Fe2TiO4 and Mg2TiO4 with Implications for Titanomagnetite Inclusions in Superdeep Diamonds"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303003136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A Present State and Perspective on Numerical Simulation Studies of Stagnant Slabs"},{"@language":"ja","@value":"滞留スラブの数値シミュレーション研究の現状と今後の展望"},{"@language":"ja-Kana","@value":"タイリュウ スラブ ノ スウチ シミュレーション ケンキュウ ノ ゲンジョウ ト コンゴ ノ テンボウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303004160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"High-Pressure Experimental Studies of Mantle Phase Transitions"},{"@language":"ja","@value":"高圧実験とマントルの相転移"},{"@language":"ja-Kana","@value":"コウアツ ジッケン ト マントル ノ ソウ テンイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679357291904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Pressure Determination by Simultaneous Ultrasonic and in situ X-ray Measurement at High Pressures and High Temperatures: MgO as an Example"},{"@language":"ja","@value":"高温高圧下におけるＭｇＯの弾性波速度，Ｘ線回折同時測定による圧力決定"},{"@language":"ja-Kana","@value":"コウオン コウアツカ ニ オケル MgO ノ ダンセイハ ソクド Xセン カイセツ ドウジ ソクテイ ニ ヨル アツリョク ケッテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681501709696","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"主要マントル鉱物の高温高圧物性と実験地球物理学"},{"@language":"en","@value":"Experimental geophysics—measurement of physical and chemical properties of major mantle minerals at high pressures and temperatures"},{"@value":"日本鉱物科学会賞第14回受賞者 受賞記念研究紹介 主要マントル鉱物の高温高圧物性と実験地球物理学"},{"@language":"ja-Kana","@value":"ニホン コウブツ カガクカイショウ ダイ14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 シュヨウ マントル コウブツ ノ コウオン コウアツ ブッセイ ト ジッケン チキュウ ブツリガク"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942123796608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Melting phase relations in the MgSiO3–CaSiO3 system at 24 Gpa"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2003jb002562"},{"@type":"OPENAIRE","@value":"doi_dedup___::83b70300b5befb426821da8aef03c8ba"},{"@type":"CROSSREF","@value":"10.1002/2013jb010466_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1002/9781118992487.ch21_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1007/s00269-017-0939-5_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1029/2008jb006222_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1134/s0869591118060048_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1186/s40645-017-0149-2_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1038/s41561-023-01169-4_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1080/08957959.2022.2112677_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2023.118197_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1002/2013je004593_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1038/s41598-018-24832-y_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2011.06.023_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2019.106348_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2011.01.008_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1029/2008jb005813_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1029/2011jb008988_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1002/2013jb010315_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1007/s00269-016-0836-3_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1029/2010gl043491_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.4131/jshpreview.20.262_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.2465/gkk.161209_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1038/s41586-021-04157-z_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1029/2018gl078960_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1029/2011jb008989_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1002/2015jb012211_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1007/s00269-016-0834-5_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1146/annurev-earth-053018-060305_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1029/2018jb016749_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2013.09.001_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.4294/zisin.61.265_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.4294/zisin.61.273_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.3389/feart.2020.00117_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1029/2019jb017704_references_DOI_YZKJoaZGIezAnUyJVA5O40R94Hf"},{"@type":"CROSSREF","@value":"10.1038/s41561-023-01244-w_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1038/s41561-019-0452-1_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1029/2018jb016924_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2016.12.045_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2013.06.005_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2012.02.009_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2017.10.005_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.1016/b978-0-444-53802-4.00054-3_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"},{"@type":"CROSSREF","@value":"10.3390/min9100614_references_DOI_DulfZvhInHMq9t1hjHxDvcCQAGY"}]}