{"@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/1361418520183048576.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/0377-0273(92)90046-g"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:037702739290046G?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:037702739290046G?httpAccept=text/plain"}}],"dc:title":[{"@value":"A review on phreatic eruptions and their precursors"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004053975555724","@type":"Researcher","foaf:name":[{"@value":"F. Barberi"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520183048577","@type":"Researcher","foaf:name":[{"@value":"A. Bertagnini"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520183048576","@type":"Researcher","foaf:name":[{"@value":"P. Landi"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520183048578","@type":"Researcher","foaf:name":[{"@value":"C. Principe"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"03770273"}],"prism:publicationName":[{"@value":"Journal of Volcanology and Geothermal Research"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1992-10","prism:volume":"52","prism:number":"4","prism:startingPage":"231","prism:endingPage":"246"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:037702739290046G?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:037702739290046G?httpAccept=text/plain"}],"createdAt":"2003-08-08","modifiedAt":"2021-06-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001201938270208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A heating process of Kuchi-erabu-jima volcano, Japan, as inferred from geomagnetic field variations and electrical structure"}]},{"@id":"https://cir.nii.ac.jp/crid/1050011804525205248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Raman microspectroscopic study of reference clay minerals and alteration minerals in volcanic ejecta from the 7 March 2012 phreatic eruption on Ioto Island (Iwo-jima), Izu-Bonin arc, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050025031478354944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Volcanic plume measurements using a UAV for the 2014 Mt. Ontake eruption"}]},{"@id":"https://cir.nii.ac.jp/crid/1050845763857360128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Reconstruction of a phreatic eruption on 27 September 2014 at Ontake volcano, central Japan, based on proximal pyroclastic density current and fallout deposits"}]},{"@id":"https://cir.nii.ac.jp/crid/1050852870543559424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The 2018 phreatic eruption at Mt. Motoshirane of Kusatsu–Shirane volcano, Japan: Eruption and intrusion of hydrothermal fluid observed by a borehole tiltmeter network"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232342644864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Resistivity structure and geochemistry of the Jigokudani Valley hydrothermal system, Mt. Tateyama, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005744245266688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Time Variation in the Chemical and Isotopic Composition of Fumarolic Gasses at Kusatsu-Shirane Volcano, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168844217088","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Quantitative Assessment of Temporal Changes in Subaqueous Hydrothermal Activity in Active Crater Lakes During Unrest Based on a Time-Series of Lake Water Chemistry"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643801576832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Groundwater Interacting at Depth With Hot Plastic Magma Triggers Phreatic Eruptions at Yugama Crater Lake of Kusatsu-Shirane Volcano (Japan)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302865554821376","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Chemical and thermal changes in hot spring waters and fumarolic gases related to volcanic unrest at Meakandake volcano, Japan: Results of long-term geochemical monitoring from 1986 to 2022"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092600395648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Imaging the Source Region of the 2015 Phreatic Eruption at Owakudani, Hakone Volcano, Japan, Using High‐Density Audio‐Frequency Magnetotellurics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092725895424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Shallow Magmatic Hydrothermal Eruption in April 2018 on Ebinokogen Ioyama Volcano in Kirishima Volcano Group, Kyushu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584340540818688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Heat transport process associated with the 2021 eruption of Aso volcano revealed by thermal and gas monitoring"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640249386240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Magma-hydrothermal system interaction inferred from volcanic gas measurements obtained during 2003–2008 at Meakandake volcano, Hokkaido, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640846539136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"First detection of precursory ground inflation of a small phreatic eruption by InSAR"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640987231488","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evolution of volcanic gas composition during repeated culmination of volcanic activity at Kuchinoerabujima volcano, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848658460187008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ten-year helium anomaly prior to the 2014 Mt Ontake eruption"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593775082752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geologic and petrologic evolution of subvolcanic hydrothermal system: A case on pyroclastic deposits since the 1331 CE eruption at Azuma-Jododaira volcano, central Fukushima, North-Eastern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861707121283840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Phreatic volcanic eruption preceded by observable shallow groundwater flow at Iwo-Yama, Kirishima Volcanic Complex, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518889286016","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Heat source of the 2014 phreatic eruption of Mount Ontake, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205196656512","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"有珠火山2000年噴火でのマグマ水蒸気爆発と火砕流到達域予測"},{"@language":"en","@value":"The 2000 eruption of Usu Volcano, Japan: characteristics of phreatomagmatic explosions and hazard evaluation for pyroclastic density currents."},{"@value":"有珠火山2000年噴火でのマグマ水蒸気爆発と火砕流到達城予測"},{"@language":"ja-Kana","@value":"ウス カザン 2000ネン フンカ デ ノ マグマ スイジョウキ バクハツ ト カサイリュウ トウタツジョウ ヨソク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206241503616","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Establishment of a high-resolution tephro-stratigraphy and chronology based on geological survey"},{"@language":"ja","@value":"地質調査による高分解能なテフラ層序学・年代学の構築"},{"@language":"ja-Kana","@value":"チシツ チョウサ ニ ヨル コウブンカイノウ ナ テフラソウ ジョガク ・ ネンダイガク ノ コウチク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288041883008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geological study of phreatic eruptions"},{"@language":"ja","@value":"水蒸気噴火の地質学的研究"},{"@language":"ja-Kana","@value":"スイジョウキ フンカ ノ チシツガクテキ ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288145330048","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The nature and source of the volcanic ash during the 2015 small phreatic eruption at Hakone volcano, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288151341824","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Electromagnetic Observations at Taal Volcano"}]},{"@id":"https://cir.nii.ac.jp/crid/1390009404771057536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Observations of Hydrothermal System and Preparatory Process of Phreatic Eruption: Recent Developments and Future Prospects"},{"@language":"ja","@value":"水蒸気噴火の発生場と噴火過程の観測"},{"@value":"水蒸気噴火の発生場と噴火過程の観測 : 最近の進展と今後の展望"},{"@language":"ja-Kana","@value":"スイジョウキ フンカ ノ ハッセイジョウ ト フンカ カテイ ノ カンソク : サイキン ノ シンテン ト コンゴ ノ テンボウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489729152","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Decade-long study of degassing at Kudriavy volcano, Iturup, Kurile Islands (1990-1999): Gas temperature and composition variations, and occurrence of 1999 phreatic eruption"}]},{"@id":"https://cir.nii.ac.jp/crid/1390290879747787648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Overview of the Special Issue “Mechanism of Phreatic Eruptions and Challenges for Eruption Forecasting: Latest Advances and Volcanic Disaster Prevention”"}]},{"@id":"https://cir.nii.ac.jp/crid/1390290879762529664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Structure of Shallow Hydrothermal System in Hakone Volcano, Japan, Inferred from Surface Displacements"},{"@language":"ja","@value":"地表面変位から推定される箱根火山浅部熱水系の構造"},{"@language":"ja-Kana","@value":"チヒョウメン ヘンイ カラ スイテイ サレル ハコネ カザンセンブ ネッスイケイ ノ コウゾウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390574411905754368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Numerical Modeling of a Volcanic Hydrothermal System Based on Resistivity Structure"}]},{"@id":"https://cir.nii.ac.jp/crid/1390845712971122816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Kusatsu-Shirane volcano as a site of phreatic eruptions"},{"@language":"ja","@value":"水蒸気噴火発生場としての草津白根火山"},{"@language":"ja-Kana","@value":"スイジョウキ フンカ ハッセイジョウ ト シテ ノ クサツ シロネ カザン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390845713026906368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Phreatomagmatic eruptions of 2014 and 2015 in Kuchinoerabujima Volcano triggered by a shallow intrusion of magma"}]},{"@id":"https://cir.nii.ac.jp/crid/1390853829701186944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Mechanisms of Steam-blast Eruptions Inferred from the Mineralogy of Volcanic Ash"},{"@language":"ja","@value":"火山灰中の鉱物からみた水蒸気噴火のメカニズム"},{"@language":"ja-Kana","@value":"カザンバイ チュウ ノ コウブツ カラ ミタ スイジョウキ フンカ ノ メカニズム"}]},{"@id":"https://cir.nii.ac.jp/crid/1390853829711100288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Preface for the Special Issue “Mechanism of Phreatic Eruptions and Challenges for Eruption Forecasting: Latest Advances and Volcanic Disaster Prevention”"},{"@language":"ja","@value":"特集号「水蒸気噴火のメカニズムと噴火予知への課題─最新の知見と火山防災─」巻頭言"},{"@value":"特集号「水蒸気噴火のメカニズムと噴火予知への課題 : 最新の知見と火山防災」巻頭言"},{"@language":"ja-Kana","@value":"トクシュウゴウ 「 スイジョウキ フンカ ノ メカニズム ト フンカ ヨチ エ ノ カダイ : サイシン ノ チケン ト カザン ボウサイ 」 カントウ ゲン"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417117557248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Quantitative relationship between plume emission and multiple deflations after the 2014 phreatic eruption at Ontake volcano, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892082785792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Chronology of the 2015 eruption of Hakone volcano, Japan : geological background, mechanism of volcanic unrest and disaster mitigation measures during the crisis"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367116819712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Imaging the hydrothermal system beneath the Jigokudani valley, Tateyama volcano, Japan : implications for structures controlling repeated phreatic eruptions from an audio-frequency magnetotelluric survey"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367119613824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Preparatory and precursory processes leading up to the 2014 phreatic eruption of Mount Ontake, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842036215936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Precursory tilt changes associated with a phreatic eruption of the Hakone volcano and the corresponding source model"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792008801024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Behavior of magmatic components in fumarolic gases related to the 2018 phreatic eruption at Ebinokogen Ioyama volcano, Kirishima Volcanic Group, Kyushu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266961891584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Infrasonic wave accompanying a crack opening during the 2015 Hakone eruption"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/0377-0273(92)90046-g"},{"@type":"CROSSREF","@value":"10.1186/s40623-016-0418-0_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.20965/jdr.2015.p0099_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1186/s40623-018-0844-2_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.3389/feart.2019.00249_references_DOI_TkJfCNPupod5DPHfaGzXH1xNhVs"},{"@type":"CROSSREF","@value":"10.1016/j.vibspec.2021.103247_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.2343/geochemj.2.0560_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01475-4_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.3389/feart.2021.740671_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1016/j.jvolgeores.2016.06.010_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.9795/bullgsj.52.231_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1186/s40623-014-0169-8_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1124-5_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.2328/jnds.37.67_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.5026/jgeography.130.811_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.5026/jgeography.130.731_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.3389/feart.2021.741742_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1016/j.jvolgeores.2023.107934_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1186/s40623-018-0887-4_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2011.0003_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2017.0071_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1029/2020gl091568_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01405-4_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.3390/geosciences10050183_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.5026/jgeography.130.797_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1186/s40623-024-01984-y_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1007/s00445-020-1358-x_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1007/s00445-011-0463-2_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1186/bf03353032_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1186/s40623-015-0288-x_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1186/s40623-016-0449-6_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1038/srep13069_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1186/s40623-018-0820-x_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1016/j.jvolgeores.2011.01.011_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1016/j.jvolgeores.2009.11.002_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.5026/jgeography.130.719_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.5026/jgeography.130.725_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1016/j.jvolgeores.2021.107274_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.20965/jdr.2022.p0654_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1038/s43247-022-00515-5_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2018.03.041_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2017.0060_references_DOI_59xsnuvRwBljDbOpBEmvaoGswHY"}]}