{"@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/1362262945951775488.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/0016-7037(95)00391-6"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0016703795003916?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0016703795003916?httpAccept=text/plain"}}],"dc:title":[{"@value":"fractionation in the system methane-hydrogen-water"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380008289873159564","@type":"Researcher","foaf:name":[{"@value":"Y. Horibe"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262945951775489","@type":"Researcher","foaf:name":[{"@value":"H. Craig"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00167037"}],"prism:publicationName":[{"@value":"Geochimica et Cosmochimica Acta"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1995-12","prism:volume":"59","prism:number":"24","prism:startingPage":"5209","prism:endingPage":"5217"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:0016703795003916?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:0016703795003916?httpAccept=text/plain"}],"createdAt":"2002-07-25","modifiedAt":"2020-02-04","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050292726798936192","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"Isotopic variation of molecular hydrogen in 20°–375°C hydrothermal fluids as detected by a new analytical method"},{"@value":"Isotopic variation of molecular hydrogen in 20–375°C hydrothermal fluids as detected by a new analytical method"}]},{"@id":"https://cir.nii.ac.jp/crid/1050577354309488896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Characteristics and varieties of gases enclathrated in natural gas hydrates retrieved at Lake Baikal"}]},{"@id":"https://cir.nii.ac.jp/crid/1050583402767224704","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Mechanoradical H2 generation during simulated faulting: Implications for an earthquake‐driven subsurface biosphere"},{"@value":"Mechanoradical H<sub>2</sub>generation during simulated faulting: Implications for an earthquake-driven subsurface biosphere"},{"@value":"Mechanoradical H2 generation during simulated faulting: implications for an earthquake-driven subsurface biosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1050862699868055936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Deep-biosphere methane production stimulated by geofluids in the Nankai accretionary complex"},{"@value":"Adsorption isotope effects of water on mesoporous silica and alumina with implications for the land-vegetation-atmosphere system"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232166617728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Hydrogen isotope systematics among H2–H2O–CH4 during the growth of the hydrogenotrophic methanogen Methanothermobacter thermautotrophicus strain ΔH"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232166800256","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Methane sources and sinks in continental sedimentary systems: New insights from paired clumped isotopologues 13CH3D and 12CH2D2"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168750770944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A Geochemical Comparison of Three Terrestrial Sites of Serpentinization: The Tablelands, the Cedars, and Aqua de Ney"}]},{"@id":"https://cir.nii.ac.jp/crid/1360016862142491392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The origin of methane in serpentinite-hosted hyperalkaline hot spring at Hakuba Happo, Japan: Radiocarbon, methane isotopologue and noble gas isotope approaches"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182088755456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Origin of methane in serpentinite-hosted hydrothermal systems: The CH4–H2–H2O hydrogen isotope systematics of the Hakuba Happo hot spring"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567185472062720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Fluid chemistry in the Solitaire and Dodo hydrothermal fields of the Central Indian Ridge"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848656901618816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Linking serpentinization, hyperalkaline mineral waters and abiotic methane production in continental peridotites: an integrated hydrogeological-bio-geochemical model from the Cabeço de Vide CH4-rich aquifer (Portugal)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657346496000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"δ13C–δD distribution of lipid biomarkers in a bacterial mat from a hot spring in Miyagi Prefecture, NE Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848659848692480","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Deepest and hottest hydrothermal activity in the Okinawa Trough: the Yokosuka site at Yaeyama Knoll"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204550098304","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fluid inclusions and their stable isotope geochemistry of the carbonate-hosted talc deposits near the Cretaceous Muamsa Granite, South Korea"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204552173824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Methane production and accumulation in the Nankai accretionary prism: Results from IODP Expeditions 315 and 316"},{"@value":"Gas Chemistry of Pore Fluids from Oomine Ridge on the Nankai Accretionary Prism"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204553019904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Hydrothermal fluid geochemistry at the Iheya North field in the mid-Okinawa Trough: Implication for origin of methane in subseafloor fluid circulation systems"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204554518400","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Mineralogy, fluid inclusion and stable isotope constraints on the genesis of the Namseong Au-Ag deposit, Republic of Korea"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288156091520","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Compositional and isotopic characteristics of hydrocarbons generated by a hydrothermal experiment simulating seafloor sediment alteration stepwise heating from 275 to 361°C at 30 MPa"}]},{"@id":"https://cir.nii.ac.jp/crid/1390859403634054528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Deep Subseafloor Biogeochemical Processes and Microbial Populations Potentially Associated with the 2011 Tohoku-oki Earthquake at the Japan Trench Accretionary Wedge (IODP Expedition 343)"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307416977929728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Hydrogen and carbon isotope systematics in hydrogenotrophic methanogenesis under H2-limited and H2-enriched conditions : implications for the origin of methane and its isotopic diagnosis"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/0016-7037(95)00391-6"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2018.10.030_references_DOI_QBPIvtZoOsAVR3MK4ynaSIPbaoA"},{"@type":"CROSSREF","@value":"10.2343/geochemj.40.69_references_DOI_QBPIvtZoOsAVR3MK4ynaSIPbaoA"},{"@type":"CROSSREF","@value":"10.1016/j.apgeochem.2018.07.011_references_DOI_QBPIvtZoOsAVR3MK4ynaSIPbaoA"},{"@type":"CROSSREF","@value":"10.1029/2021jg006316_references_DOI_QBPIvtZoOsAVR3MK4ynaSIPbaoA"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2022.117510_references_DOI_QBPIvtZoOsAVR3MK4ynaSIPbaoA"},{"@type":"CROSSREF","@value":"10.2343/geochemj.1.0105_references_DOI_QBPIvtZoOsAVR3MK4ynaSIPbaoA"},{"@type":"CROSSREF","@value":"10.1016/j.orggeochem.2009.11.008_references_DOI_QBPIvtZoOsAVR3MK4ynaSIPbaoA"},{"@type":"CROSSREF","@value":"10.1007/978-90-481-8885-7_12_references_DOI_QBPIvtZoOsAVR3MK4ynaSIPbaoA"},{"@type":"CROSSREF","@value":"10.1029/2009jg001203_references_DOI_QBPIvtZoOsAVR3MK4ynaSIPbaoA"},{"@type":"CROSSREF","@value":"10.1029/2011gl048850_references_DOI_QBPIvtZoOsAVR3MK4ynaSIPbaoA"},{"@type":"CROSSREF","@value":"10.1111/gfl.12201_references_DOI_QBPIvtZoOsAVR3MK4ynaSIPbaoA"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2014.07.020_references_DOI_QBPIvtZoOsAVR3MK4ynaSIPbaoA"},{"@type":"CROSSREF","@value":"10.1264/jsme2.me22108_references_DOI_QBPIvtZoOsAVR3MK4ynaSIPbaoA"},{"@type":"CROSSREF","@value":"10.1186/s40645-016-0088-3_references_DOI_QBPIvtZoOsAVR3MK4ynaSIPbaoA"},{"@type":"CROSSREF","@value":"10.1098/rsos.171570_references_DOI_QBPIvtZoOsAVR3MK4ynaSIPbaoA"},{"@type":"CROSSREF","@value":"10.1126/sciadv.aao4631_references_DOI_QBPIvtZoOsAVR3MK4ynaSIPbaoA"},{"@type":"CROSSREF","@value":"10.2343/geochemj.2.0245_references_DOI_QBPIvtZoOsAVR3MK4ynaSIPbaoA"},{"@type":"CROSSREF","@value":"10.1038/s41598-023-31669-7_references_DOI_QBPIvtZoOsAVR3MK4ynaSIPbaoA"},{"@type":"CROSSREF","@value":"10.2343/geochemj.2.0566_references_DOI_QBPIvtZoOsAVR3MK4ynaSIPbaoA"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2013.11.001_references_DOI_QBPIvtZoOsAVR3MK4ynaSIPbaoA"}]}