{"@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/1390282681523089152.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2465/jmps.150829"}},{"identifier":{"@type":"URI","@value":"https://www.jstage.jst.go.jp/article/jmps/111/2/111_150829/_pdf"}},{"identifier":{"@type":"NAID","@value":"130005150438"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@language":"en","@value":"Peak and post–peak development of UHT metamorphism at Mather Peninsula, Rauer Islands: Zircon and monazite U–Th–Pb and REE chemistry constraints"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"Zircon and monazite in ultrahigh temperature (UHT) metamorphic rocks from the Rauer Islands of Prydz Bay in East Antarctica were investigated in terms of U–Th–Pb and rare earth elements (REE) chemistry along with textural context. All five analyzed samples, three from the Mather Paragneiss UHT unit and two from the host orthogneiss unit yield 522–517 Ma concordant zircon ages, with older protolith/inherited zircon ages of 3268 and 2800–2400 Ma along with highly discordant Mesoproterozoic to Neoproterozoic ages. Our data confirm the Archaean protolith age for the host orthogneiss surrounding the UHT Mather Paragneiss. The Archaean and Mesoproterzoic components of the Rauer Islands were not amalgamated in the Rauer Tectonic Event at 1030–990 Ma, and deposition of the Mather Paragneiss was considered at some time after the Rauer Tectonic Event. In contrast to the well–defined 520 Ma ages obtained from the zircons in the UHT rocks, monazite grains measured by electron microprobe show a distinct internal zonation, from 580–560 Ma dark–backscattered electron image (BSE) cores enriched in middle rare earth elements (MREE) and heavy rare earth elements (HREE) to 550–520 Ma mid–BSE mantles and 510–500 Ma bright–BSE rims. From the chemical and textural evidence we infer that the MREE–HREE–rich 580–560 Ma monazite cores may have formed through the decomposition of garnet during decompression just after the UHT event, whereas the MREE–HREE–depleted 550–500 Ma monazite grains/rims formed or recrystallized in reactions associated with subsequent extensive hydration during the upper–amphibolite to granulite–facies main Prydz Tectonic Event, which also caused marked recrystallization of zircon. The above data strongly support the interpretation that the UHT metamorphism occurred prior to 590–580 Ma."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420564276165004544","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"60370095"},{"@type":"NRID","@value":"1000060370095"},{"@type":"NRID","@value":"9000001319467"},{"@type":"NRID","@value":"9000002384333"},{"@type":"NRID","@value":"9000323295379"},{"@type":"NRID","@value":"9000402491996"},{"@type":"NRID","@value":"9000370280902"},{"@type":"NRID","@value":"9000401432630"},{"@type":"NRID","@value":"9000258414543"},{"@type":"NRID","@value":"9000258434590"},{"@type":"NRID","@value":"9000258433463"},{"@type":"NRID","@value":"9000000056129"},{"@type":"NRID","@value":"9000347190988"},{"@type":"NRID","@value":"9000258005089"},{"@type":"NRID","@value":"9000258414551"},{"@type":"NRID","@value":"9000017482953"},{"@type":"NRID","@value":"9000002207111"},{"@type":"NRID","@value":"9000397721152"},{"@type":"NRID","@value":"9000366131005"},{"@type":"NRID","@value":"9000347137250"},{"@type":"NRID","@value":"9000347192083"},{"@type":"NRID","@value":"9000414374293"},{"@type":"NRID","@value":"9000001806967"},{"@type":"NRID","@value":"9000333112773"},{"@type":"NRID","@value":"9000347191901"},{"@type":"NRID","@value":"9000323295399"},{"@type":"NRID","@value":"9000347082822"},{"@type":"NRID","@value":"9000019982717"},{"@type":"NRID","@value":"9000347192072"},{"@type":"NRID","@value":"9000392820592"},{"@type":"NRID","@value":"9000347135506"},{"@type":"NRID","@value":"9000017395839"},{"@type":"NRID","@value":"9000020136182"},{"@type":"NRID","@value":"9000347138241"},{"@type":"NRID","@value":"9000347082818"},{"@type":"NRID","@value":"9000347190994"},{"@type":"NRID","@value":"9000347167066"},{"@type":"NRID","@value":"9000258417804"},{"@type":"NRID","@value":"9000258415474"},{"@type":"NRID","@value":"9000335196143"},{"@type":"NRID","@value":"9000370280966"},{"@type":"NRID","@value":"9000283726171"},{"@type":"NRID","@value":"9000258433297"},{"@type":"NRID","@value":"9000258433392"},{"@type":"NRID","@value":"9000290381407"},{"@type":"NRID","@value":"9000290381406"},{"@type":"NRID","@value":"9000405027380"},{"@type":"NRID","@value":"9000310331235"},{"@type":"NRID","@value":"9000347082171"},{"@type":"NRID","@value":"9000258433958"},{"@type":"NRID","@value":"9000258434680"},{"@type":"NRID","@value":"9000405098868"},{"@type":"NRID","@value":"9000283728177"},{"@type":"NRID","@value":"9000350560740"},{"@type":"NRID","@value":"9000396138758"},{"@type":"NRID","@value":"9000405027458"},{"@type":"NRID","@value":"9000258434586"},{"@type":"NRID","@value":"9000347135747"},{"@type":"NRID","@value":"9000001848202"},{"@type":"NRID","@value":"9000317561466"},{"@type":"NRID","@value":"9000347191925"},{"@type":"NRID","@value":"9000345427416"},{"@type":"NRID","@value":"9000323295384"},{"@type":"NRID","@value":"9000283783532"},{"@type":"NRID","@value":"9000347082775"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/thokada"}],"foaf:name":[{"@language":"en","@value":"HOKADA Tomokazu"}],"jpcoar:affiliationName":[{"@language":"en","@value":"National Institute of Polar Research"},{"@language":"en","@value":"Department of Polar Science, SOKENDAI (The Graduate University for Advanced Studies)"},{"@language":"en","@value":"School of Geosciences, University of Edinburgh"},{"@language":"en","@value":"Department of Geology and Paleontology, National Museum of Nature and Science"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282681523089152","@type":"Researcher","foaf:name":[{"@language":"en","@value":"DUNKLEY Daniel J."}],"jpcoar:affiliationName":[{"@language":"en","@value":"National Institute of Polar Research"},{"@language":"en","@value":"Department of Applied Geology, Curtin University"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282681523089156","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000323295385"}],"foaf:name":[{"@language":"en","@value":"HARLEY Simon L."}],"jpcoar:affiliationName":[{"@language":"en","@value":"School of Geosciences, University of Edinburgh"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282681523089154","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000323295387"}],"foaf:name":[{"@language":"en","@value":"KELLY Nigel M."}],"jpcoar:affiliationName":[{"@language":"en","@value":"School of Geosciences, University of Edinburgh"},{"@language":"en","@value":"Department of Geological Sciences, University of Colorado"}]},{"@id":"https://cir.nii.ac.jp/crid/1030003658399285248","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"40126628"},{"@type":"NRID","@value":"1000040126628"},{"@type":"NRID","@value":"9000257887677"},{"@type":"NRID","@value":"9000401431440"},{"@type":"NRID","@value":"9000002468181"},{"@type":"NRID","@value":"9000243883329"},{"@type":"NRID","@value":"9000401432722"},{"@type":"NRID","@value":"9000257979543"},{"@type":"NRID","@value":"9000296661827"},{"@type":"NRID","@value":"9000370745965"},{"@type":"NRID","@value":"9000272993657"},{"@type":"NRID","@value":"9000020084584"},{"@type":"NRID","@value":"9000020178572"},{"@type":"NRID","@value":"9000323295388"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0179577"}],"foaf:name":[{"@language":"en","@value":"YOKOYAMA Kazumi"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Department of Geology and Paleontology, National Museum of Nature and Science"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"13456296"},{"@type":"LISSN","@value":"13456296"},{"@type":"EISSN","@value":"13493825"}],"prism:publicationName":[{"@language":"en","@value":"Journal of Mineralogical and Petrological Sciences"},{"@language":"en","@value":"Journal of Mineralogical and Petrological Sciences"}],"dc:publisher":[{"@language":"en","@value":"Japan Association of Mineralogical Sciences"},{"@language":"ja","@value":"一般社団法人　日本鉱物科学会"}],"prism:publicationDate":"2016","prism:volume":"111","prism:number":"2","prism:startingPage":"89","prism:endingPage":"103"},"reviewed":"false","url":[{"@id":"https://www.jstage.jst.go.jp/article/jmps/111/2/111_150829/_pdf"}],"availableAt":"2016","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Monazite","dc:title":"Monazite"},{"@id":"https://cir.nii.ac.jp/all?q=Rare%20earth%20elements%20(REE)","dc:title":"Rare earth elements (REE)"},{"@id":"https://cir.nii.ac.jp/all?q=Ultrahigh%20temperature%20(UHT)%20metamorphism","dc:title":"Ultrahigh temperature (UHT) metamorphism"},{"@id":"https://cir.nii.ac.jp/all?q=U%E2%80%93Th%E2%80%93Pb%20geochronology","dc:title":"U–Th–Pb geochronology"},{"@id":"https://cir.nii.ac.jp/all?q=Zircon","dc:title":"Zircon"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040282256806039168","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15H03748"},{"@type":"JGN","@value":"JP15H03748"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15H03748/"}],"notation":[{"@language":"ja","@value":"マントル組成変化と大陸衝突事変に基づく地殻・マントル物質循環の精密解析"},{"@language":"en","@value":"Crust-mantle interaction and compositional variation of continental lithosphere due to collision event"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282256821677056","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15K05312"},{"@type":"JGN","@value":"JP15K05312"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15K05312/"}],"notation":[{"@language":"ja","@value":"超大陸分裂開始時における高Ｋアダカイト－閃長岩複合火成活動の意義"},{"@language":"en","@value":"Geological significance of high-K adakitic granite and syenite complex in the early stage of continental break-up"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257219898240","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"25287132"},{"@type":"JGN","@value":"JP25287132"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-25287132/"}],"notation":[{"@language":"ja","@value":"地殻形成素過程解明に向けた微小領域高精度ジルコン年代測定の実証研究"},{"@language":"en","@value":"Geochronological study of high precision zircon microanalysis for crustal evolution"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257223703552","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"25302008"},{"@type":"JGN","@value":"JP25302008"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-25302008/"}],"notation":[{"@language":"ja","@value":"後期太古代氷河期における汎地球的な環境変動の解明：同位体地質学からのアプローチ"},{"@language":"en","@value":"Geological and isotopic record of Late Archean glaciation and global environmental changes"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257230930688","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"25400518"},{"@type":"JGN","@value":"JP25400518"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-25400518/"}],"notation":[{"@language":"ja","@value":"低圧変成帯の温度圧力構造と島弧地殻のダイナミクスの解明"},{"@language":"en","@value":"Thermobaric structure of low-pressure metamorphic belts and dynamics of crust beneath island arcs"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360011145068359936","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The impact of zircon–garnet REE distribution data on the interpretation of zircon U–Pb ages in complex high-grade terrains: An example from the Rauer Islands, East Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145879418368","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Approximation of terrestrial lead isotope evolution by a two-stage model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360282588972956032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Zircon Behaviour and the Thermal Histories of Mountain Chains"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619201122560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Experimental zircon/melt and zircon/garnet trace element partitioning and implications for the geochronology of crustal rocks"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619526980608","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the application of\n            <i>in situ</i>\n            monazite chemical geochronology to constraining\n            <i>P</i>\n            –\n            <i>T</i>\n            –\n            <i>t</i>\n            histories in high-temperature (\n            <b>></b>\n            850\n            <b>°</b>\n            C) polymetamorphic granulites from Prydz Bay, East Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621464449152","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Antarctica and supercontinent evolution: historical perspectives, recent advances and unresolved issues"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094298344960","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"SHRIMP zircon age constraints from the Larsemann Hills region, Prydz Bay, for a late Mesoproterozoic to early Neoproterozoic tectono-thermal event in East Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118820493312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Timing, Duration and Conditions of UHT Metamorphism in Remnants of the Former Eastern Gondwana"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043618358400","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"U‐Pb geochronology of zircons from lunar breccia 73217 using a sensitive high mass‐resolution ion microprobe"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137044699516928","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Discovery of a Neoproterozoic basin in the Prydz belt in East Antarctica and its implications for Gondwana assembly and ultrahigh temperature metamorphism"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045158338048","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geochronology of the khondalite belt of Trivandrum Block, Southern India: Electron probe ages and implications for Gondwana tectonics"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045600298880","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Pressure–temperature evolution of metapelitic granulites in a polymetamorphic terrane: the Rauer Group, East Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418521385286272","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Two stages of zircon and monazite growth in anatectic leucogneiss: SHRIMP constraints on the duration and intensity of Pan‐African metamorphism in Prydz Bay, East Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994796007552","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"SHRIMP and electron microprobe chronology of UHT metamorphism in the Napier Complex, East Antarctica: implications for zircon growth at >1,000��C"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995388815744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Boron- and phosphate-rich rocks in the Larsemann Hills, Prydz Bay, East Antarctica: tectonic implications"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995974072320","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Pan‐African granulite facies metamorphic episode in Prydz Bay, Antarctica: Evidence from Sm‐Nd garnet dating"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468531015808","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"SHRIMP U–Pb zircon geochronology of high-grade rocks and charnockites from the eastern Amery Ice Shelf and southwestern Prydz Bay, East Antarctica: Constraints on Late Mesoproterozoic to Cambrian tectonothermal events related to supercontinent assembly"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981469761201280","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Chapter 3.2 Ancient Antarctica: The Archaean of the East Antarctic Shield"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470060832128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"New constraints on metamorphism in the Rauer Group, Prydz Bay, east Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470247683072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Proterozoic basement provinces of southern and southwestern Australia, and their correlation with Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470778238464","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Abundances of the elements: Meteoritic and solar"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981471353893888","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"(Th+U)-Pb monazite ages from Al-Mg-rich metapelites, Rauer Group, east Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943310248832","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Precise U‐Pb ages of Duluth Complex and related mafic intrusions, northeastern Minnesota: Geochronological insights to physical, petrogenetic, paleomagnetic, and tectonomagmatic processes associated with the 1.1 Ga Midcontinent Rift System"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943713959808","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Zircon ages and the distribution of Archaean and Proterozoic rocks in the Rauer Islands"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945376693888","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Grenville-age basement provinces in East Antarctica: Evidence for three separate collisional orogens"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544418675363200","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Timing of the progress granite, Larsemann hills: Additional evidence for early Palaeozoic orogenesis within the east Antarctic Shield and implications for Gondwana assembly"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419051556480","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"New constraints from U–Pb, Lu–Hf and Sm–Nd isotopic data on the timing of sedimentation and felsic magmatism in the Larsemann Hills, Prydz Bay, East Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420622710272","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Middle precambrian provenance of Jurassic sandstone in the Mino Terrane, central Japan: Th-U-total Pb evidence from an electron microprobe monazite study"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893888749440","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Further Characterisation of the 91500 Zircon Crystal"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894098053504","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Precambrian geological relationships in high‐grade gneisses of the Rauer Islands, east Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894950245248","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Experimental determination of <scp>REE</scp> partition coefficients between zircon, garnet and melt: a key to understanding high‐<i>T</i> crustal processes"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895111979136","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Stable isotopic signatures of superposed fluid events in granulite facies marbles of the Rauer Group, East Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368638315648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Ultrahigh temperature granulite metamorphism (1050 °C, 12 kbar) and decompression in garnet (Mg70)–orthopyroxene–sillimanite gneisses from the Rauer Group, East Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370335030144","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Regional geochemical and isotopic characteristics of high-grade metamorphics of the Prydz bay area: The extent of proterozoic reworking of Qrchaean continental crust in East Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370933696640","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Archaean-Cambrian crustal development of East Antarctica: metamorphic characteristics and tectonic implications"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844438866816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An integrated microtextural and chemical approach to zircon geochronology: refining the Archaean history of the Napier Complex, east Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844706952320","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Antarctica — Before and after Gondwana"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844946349312","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Calculated phase equilibria in K<sub>2</sub>O‐FeO‐MgO‐Al<sub>2</sub>O<sub>3</sub>‐SiO<sub>2</sub>‐H<sub>2</sub>O for silica‐undersaturated sapphirine‐bearing mineral assemblages"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670321285817984","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The structural evolution of the Rauer Group, East Antarctica: mafic dykes as passive markers in a composite Proterozoic terrain"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951793317215616","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Constraints on the stratigraphic age of metasedimentary rocks from the Larsemann Hills, East Antarctica: possible implications for Neoproterozoic tectonics"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795096143360","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The evolution of a layered metaigneous complex in the Rauer Group, East Antarctica: evidence for a distinct Archaean terrane"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268381999616","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Metapelitic Migmatites from Brattstrand Bluffs, East Antarctica—Metamorphism, Melting and Exhumation of the Mid Crust"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268721469312","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The\n            <i>c.</i>\n            1000–900 Ma and\n            <i>c.</i>\n            550–500 Ma tectonothermal events in the Prince Charles Mountains–Prydz Bay region, East Antarctica, and their relations to supercontinent evolution"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206240097920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Recent progress in lower crustal process:"},{"@language":"ja","@value":"島弧-大陸地殻深部現象の研究進展："},{"@value":"島弧-大陸地殻深部現象の研究進展 : 超高温変成作用の精密解析"},{"@language":"ja-Kana","@value":"トウコ-タイリク チカク シンブ ゲンショウ ノ ケンキュウ シンテン : チョウコウオン ヘンセイ サヨウ ノ セイミツ カイセキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206545404288","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A matter of time: The importance of the duration of UHT metamorphism"},{"@value":"A matter of time: The importance of duration of UHT metamorphism"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206545412608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Metamorphism and continental growth: Introduction"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:2000978298"},{"@type":"CROSSREF","@value":"10.2465/jmps.150829"},{"@type":"CIA","@value":"130005150438"},{"@type":"KAKEN","@value":"PRODUCT-20822785"},{"@type":"KAKEN","@value":"PRODUCT-21371041"},{"@type":"KAKEN","@value":"PRODUCT-21000972"},{"@type":"KAKEN","@value":"PRODUCT-20619123"},{"@type":"KAKEN","@value":"PRODUCT-21005161"},{"@type":"KAKEN","@value":"PRODUCT-21247669"},{"@type":"KAKEN","@value":"PRODUCT-20633749"},{"@type":"OPENAIRE","@value":"doi_dedup___::b3b4a063b3391e47979b0dc7ca80ebf2"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2017.0059_references_DOI_CmWcW5Qd7PilBPnjgOpRBN8n1cp"},{"@type":"CROSSREF","@value":"10.1093/petrology/egab068_references_DOI_CmWcW5Qd7PilBPnjgOpRBN8n1cp"},{"@type":"CROSSREF","@value":"10.2465/jmps.160128_references_DOI_CmWcW5Qd7PilBPnjgOpRBN8n1cp"},{"@type":"CROSSREF","@value":"10.2465/jmps.160420_references_DOI_CmWcW5Qd7PilBPnjgOpRBN8n1cp"}]}