{"@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/1360004232135458816.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.epsl.2016.02.018"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X16300292?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X16300292?httpAccept=text/plain"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Origin of magnetic highs at ultramafic hosted hydrothermal systems: Insights from the Yokoniwa site of Central Indian Ridge"}],"description":[{"notation":[{"@value":"High-resolution vector magnetic measurements were performed on an inactive ultramafic-hosted hydrothermal vent field, called Yokoniwa Hydrothermal Field (YHF), using a deep-sea manned submersible Shinkai6500 and an autonomous underwater vehicle r2D4. The YHF has developed at a non-transform offset massif of the Central Indian Ridge. Dead chimneys were widely observed around the YHF along with a very weak venting of low-temperature fluids so that hydrothermal activity of the YHF was almost finished. The distribution of crustal magnetization from the magnetic anomaly revealed that the YHF is associated with enhanced magnetization, as seen at the ultramafic-hosted Rainbow and Ashadze-1 hydrothermal sites of the Mid-Atlantic Ridge. The results of rock magnetic analysis on seafloor rock samples (including basalt, dolerite, gabbro, serpentinized peridotite, and hydrothermal sulfide) showed that only highly serpentinized peridotite carries high magnetic susceptibility and that the natural remanent magnetization intensity can explain the high magnetization of Yokoniwa. These observations reflect abundant and strongly magnetized magnetite grains within the highly serpentinized peridotite. Comparisons with the Rainbow and Ashadze-1 suggest that in ultramafic-hosted hydrothermal systems, strongly magnetized magnetite and pyrrhotite form during the progression of hydrothermal alteration of peridotite. After the completion of serpentinization and production of hydrogen, pyrrhotites convert into pyrite or nonmagnetic iron sulfides, which considerably reduces their levels of magnetization. Our results revealed origins of the magnetic high and the development of subsurface chemical processes in ultramafic-hosted hydrothermal systems. Furthermore, the results highlight the use of near-seafloor magnetic field measurements as a powerful tool for detecting and characterizing seafloor hydrothermal systems."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004232135458817","@type":"Researcher","foaf:name":[{"@value":"Masakazu Fujii"}]},{"@id":"https://cir.nii.ac.jp/crid/1420564276172667648","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"30313191"},{"@type":"NRID","@value":"1000030313191"},{"@type":"ORCID","@value":"0000-0001-7070-7982"},{"@type":"NRID","@value":"9000347167234"},{"@type":"NRID","@value":"9000004619549"},{"@type":"NRID","@value":"9000338419016"},{"@type":"NRID","@value":"9000020206430"},{"@type":"NRID","@value":"9000345439026"},{"@type":"NRID","@value":"9000309997988"},{"@type":"NRID","@value":"9000017396039"},{"@type":"NRID","@value":"9000258416708"},{"@type":"NRID","@value":"9000254343174"},{"@type":"NRID","@value":"9000345426784"},{"@type":"NRID","@value":"9000347226820"},{"@type":"NRID","@value":"9000007970137"},{"@type":"NRID","@value":"9000258414050"},{"@type":"NRID","@value":"9000311505415"},{"@type":"NRID","@value":"9000347191061"},{"@type":"NRID","@value":"9000017413422"},{"@type":"NRID","@value":"9000311505440"},{"@type":"NRID","@value":"9000347137119"},{"@type":"NRID","@value":"9000258411772"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/okinokyoko"}],"foaf:name":[{"@value":"Kyoko Okino"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004232135458820","@type":"Researcher","foaf:name":[{"@value":"Taichi Sato"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004232135458819","@type":"Researcher","foaf:name":[{"@value":"Hiroshi Sato"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004232135458816","@type":"Researcher","foaf:name":[{"@value":"Kentaro Nakamura"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"0012821X"}],"prism:publicationName":[{"@value":"Earth and Planetary Science Letters"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2016-05","prism:volume":"441","prism:startingPage":"26","prism:endingPage":"37"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","http://www.elsevier.com/open-access/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0012821X16300292?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0012821X16300292?httpAccept=text/plain"}],"createdAt":"2016-03-09","modifiedAt":"2022-06-17","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Geophysics","dc:title":"Geophysics"},{"@id":"https://cir.nii.ac.jp/all?q=Space%20and%20Planetary%20Science","dc:title":"Space and Planetary Science"},{"@id":"https://cir.nii.ac.jp/all?q=Geochemistry%20and%20Petrology","dc:title":"Geochemistry and Petrology"},{"@id":"https://cir.nii.ac.jp/all?q=Earth%20and%20Planetary%20Sciences%20(miscellaneous)","dc:title":"Earth and Planetary Sciences (miscellaneous)"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781844891904","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15K05263"},{"@type":"JGN","@value":"JP15K05263"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15K05263/"}],"notation":[{"@language":"ja","@value":"海洋トランスフォーム断層を通じて地球内部に運ばれる水"},{"@language":"en","@value":"Oceanic Transform as a water inlet to earth's interior"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000782438250240","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"13J08982"},{"@type":"JGN","@value":"JP13J08982"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-13J08982/"}],"notation":[{"@language":"ja","@value":"高分解能ベクトル磁気探査による海底熱水循環系の構造と形成過程に関する研究"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282256809615872","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15H05207"},{"@type":"JGN","@value":"JP15H05207"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15H05207/"}],"notation":[{"@language":"ja","@value":"深海における地磁気異常が明らかにする古地磁気変動"},{"@language":"en","@value":"Investigation on variations of the geomagnetic paleo-intensity using deep-tow and sea-surface magnetic anomalies"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050283688373022720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Near-seafloor magnetic mapping of off-axis lava flows near the Kairei and Yokoniwa hydrothermal vent fields in the Central Indian Ridge"}]},{"@id":"https://cir.nii.ac.jp/crid/1050574201775550720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geological background of the Kairei and Edmond hydrothermal fields along the Central Indian Ridge : Implications for the distinct chemistry between their vent fluids"},{"@value":"Geological background of the Kairei and Edmond hydrothermal fields along the Central Indian Ridge: Implications of their vent fluids’ distinct chemistry"},{"@value":"Geological background of the Kairei and Edmond hydrothermal vent fields along the Central Indian Ridge: Insights into the distinct chemistry between their vent fluids"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229802630144","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"High‐resolution magnetic signature of active hydrothermal systems in the back‐arc spreading region of the southern Mariana Trough"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011143494689408","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Structural analysis of the segmentation of the Central Indian Ridge between 20�30?S and 25�30?S (Rodriguez Triple Junction)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011143853601920","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mid-Ocean Ridge Hydrothermal Fluxes and the Chemical Composition of the Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144130302592","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Magnetic study of basalts from the Mid-Atlantic Ridge, lat 37°N"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144622091264","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"High‐resolution near‐bottom vector magnetic anomalies over Raven Hydrothermal Field, Endeavour Segment, Juan de Fuca Ridge"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144881540224","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A near‐bottom magnetic survey of the Mid‐Atlantic Ridge axis at 26°N: Implications for the tectonic evolution of the TAG segment"}]},{"@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/1360292617915348480","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Magnetic properties of zero‐age oceanic crust; A new submarine lava flow on the Juan de Fuca Ridge"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292618976765440","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three‐dimensional magnetic and gravity studies of the Rodriguez Triple Junction in the Indian Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619262171520","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Central anomaly magnetization high: constraints on the volcanic construction and architecture of seismic layer 2A at a fast-spreading mid-ocean ridge, the EPR at 9°30′–50′N"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619454133632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A reduced crustal magnetization zone near the first observed active hydrothermal vent field on the Southwest Indian Ridge"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620094537344","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Variations in layer 2A thickness and the origin of the central anomaly magnetic high"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621425779072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Interaction of submarine volcanic and high-temperature hydrothermal activity proposed for the formation of the Agrokipia, volcanic massive sulfide deposits of Cyprus"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166662469376","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The inversion of deep‐sea magnetic anomalies using Akaike's Bayesian information criterion"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092887403392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geologically current plate motions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092887413760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Serpentinite-Hosted Ecosystem: The Lost City Hydrothermal Field"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094293389056","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A new shipboard three-component magnetometer"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095618882304","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global changes in intensity of the Earth's magnetic field during the past 800 kyr"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574096041921536","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seawater‐peridotite interactions: First insights from ODP Leg 209, MAR 15°N"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657031009920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Discovery of a new hydrothermal vent based on an underwater, high-resolution geophysical survey"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657065250560","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Serpentinized troctolites exposed near the Kairei Hydrothermal Field, Central Indian Ridge: Insights into the origin of the Kairei hydrothermal fluid supporting a unique microbial ecosystem"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567862883200","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Chemical characteristics of newly discovered black smoker fluids and associated hydrothermal plumes at the Rodriguez Triple Junction, Central Indian Ridge"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569820452480","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The abundance of seafloor massive sulfide deposits"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855571014900096","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Magnetic and Opaque Petrological Response of Basalts to Regional Hydrothermal Alteration"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865816813444736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geomagnetic paleointensity dating of mid-ocean ridge basalts from the neo-volcanic zone of the Central Indian Ridge"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045758774784","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"What causes low magnetization at basalt-hosted hydrothermal sites? Insights from inactive site Krasnov (MAR 16°38′N)"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137046258855168","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Interpretation of aeromagnetic anomalies in terms of hydrothermal alteration in Cretaceous normal polarity superchron extrusives of the Troodos, Cyprus, ophiolite"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519157800320","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Iron partitioning and hydrogen generation during serpentinization of abyssal peridotites from 15°N on the Mid-Atlantic Ridge"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520553608576","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Magnetic structure of a slow spreading ridge segment: Insights from near‐bottom magnetic measurements on board a submersible"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418521173672192","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A deep tow magnetic survey of Middle Valley, Juan de Fuca Ridge"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993573747328","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Compositional controls on hydrogen generation during serpentinization of ultramafic rocks"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994905837056","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Serpentinization of oceanic peridotites: 1. A high‐sensitivity method to monitor magnetite production in hydrothermal experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995300905472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Mid-Atlantic Ridge at 45° N. XIV. Oxidation and magnetic properties of basalt; review and discussion"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468504417024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"International Geomagnetic Reference Field: the eleventh generation"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468848195840","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Magnetic properties and opaque mineralogy of rocks from selected seafloor hydrothermal sites at oceanic ridges"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981469311004032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mineralogical zonation and metasomatism of the alteration pipes of Cyprus sulfide deposits"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981469570637824","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Magnetic signatures of hydrothermal alteration and volcanogenic mineral deposits in oceanic crust"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470839824512","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Igneous, Alteration and Exhumation Processes Recorded in Abyssal Peridotites and Related Fault Rocks from an Oceanic Core Complex along the Central Indian Ridge"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944474210560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Magnetic structure of an oceanic core complex at the southernmost Central Indian Ridge: Analysis of shipboard and deep‐sea three‐component magnetometer data"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945601916544","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Alteration processes at Deep Sea Drilling Project/Ocean Drilling Program Hole 504B at the Costa Rica Rift: Implications for magnetization of oceanic crust"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945967143552","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Reduced crustal magnetization beneath the active sulfide mound, TAG hydrothermal field, Mid-Atlantic Ridge at 26°N"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262946070451328","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Direct inversion of potential fields from an uneven track with application to the Mid‐Atlantic Ridge"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262946215877248","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Detachment faults at Mid‐Ocean Ridges garner interest"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544418877310720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Crustal magnetization reveals subsurface structure of Juan de Fuca Ridge hydrothermal vent fields"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893320070784","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Magnetite in seafloor serpentinite--Some like it hot"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894015418496","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Magnetic properties of variably serpentinized abyssal peridotites"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894940321024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Reduced crustal magnetization beneath Relict Hydrothermal Mounds: TAG Hydrothermal Field, Mid‐Atlantic Ridge, 26°N"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318918076672","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Vertical magnetic structure of ocean crust determined from near‐bottom magnetic field measurements"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318931175168","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Deep‐sea magnetic vector anomalies over the Hakurei hydrothermal field and the Bayonnaise knoll caldera, Izu‐Ogasawara arc, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320001888256","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The magnetic signature of ultramafic-hosted hydrothermal sites"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670321141594880","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geochemical and microbiological evidence for a hydrogen-based, hyperthermophilic subsurface lithoautotrophic microbial ecosystem (HyperSLiME) beneath an active deep-sea hydrothermal field"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268542485888","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The inversion of magnetic anomalies in the presence of topography"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268901417472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"3‐D focused inversion of near‐seafloor magnetic data with application to the Brothers volcano hydrothermal system, Southern Pacific Ocean, New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269279443200","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Relationship of the Central Indian Ridge segmentation with the evolution of the Rodrigues Triple Junction for the past 8 Myr"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269537440384","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Magnetic anomalies associated with high temperature reservoirs in the taupo volcanic zone (New Zealand)"}]},{"@id":"https://cir.nii.ac.jp/crid/1370568855667289729","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"High-resolution magnetic surveys over the Middle Valley mounds, northern Juan de Fuca Ridge"}]},{"@id":"https://cir.nii.ac.jp/crid/1370568855667289860","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tectonic background of four hydrothermal fields along the Central Indian Ridge"}]},{"@id":"https://cir.nii.ac.jp/crid/1370568855667289873","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rock magnetic properties of hydrothermally formed iron sulfides from Middle Valley, Juan de Fuca ridge"}]},{"@id":"https://cir.nii.ac.jp/crid/1370568855667289991","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"High production and fluxes of H2 and CH4 and evidence of abiotic hydrocarbon synthesis by serpentinization in ultramafic-hosted hydrothermal systems on the Mid-Atlantic Ridge"}]},{"@id":"https://cir.nii.ac.jp/crid/1370568855667290117","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Petrology and geochemistry of Mid-Ocean Ridge Basalts from the Southern Central Indian Ridge"}]},{"@id":"https://cir.nii.ac.jp/crid/1370568855667290125","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geodiversity of hydrothermal processes along the Mid-Atlantic Ridge and ultramafic-hosted mineralization: a new type of oceanic Cu–Zn–Co–Au volcanogenic massive sulfide deposit"}]},{"@id":"https://cir.nii.ac.jp/crid/1370568855667290126","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The magnetic signature of hydrothermal systems in slow spreading environments"}]},{"@id":"https://cir.nii.ac.jp/crid/1370568855667290243","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The effect of oxidation on the Verwey transition in magnetite"}]},{"@id":"https://cir.nii.ac.jp/crid/1370568855667290246","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Computation of magnetic anomalies caused by two-dimensional structures of arbitrary shape"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892134481920","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Theoretical constraints of physical and chemical properties of hydrothermal fluids on variations in chemolithotrophic microbial communities in seafloor hydrothermal systems"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.epsl.2016.02.018"},{"@type":"KAKEN","@value":"PRODUCT-21165257"},{"@type":"KAKEN","@value":"PRODUCT-20179806"},{"@type":"KAKEN","@value":"PRODUCT-20485840"},{"@type":"KAKEN","@value":"PRODUCT-20836125"},{"@type":"OPENAIRE","@value":"doi_dedup___::07101cb8de9ee3ad7d7106f1814118d2"},{"@type":"CROSSREF","@value":"10.1186/s40623-018-0959-5_references_DOI_P8TYk4rQ0UgBVzbvCHjFJci4ZQ8"},{"@type":"CROSSREF","@value":"10.1186/s40623-024-01963-3_references_DOI_P8TYk4rQ0UgBVzbvCHjFJci4ZQ8"}]}