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The observed specimens were chips (fifteen samples) and thin sections (five samples). The obtained spectra were decomposed into four components: G<sub>L</sub>, D1, D3, and D4 bands at 1600, 1350, 1510, and 1245 cm<sup>−1</sup>, respectively. The full width at half maximum of the D1 band (Γ<sub>D1</sub>) decreased with increasing peak metamorphic temperature (PMT) of the parent body, as published previously. By increasing the number of band components to four, the applicable range of the Raman spectroscopic thermometer using Γ<sub>D1</sub> extended its lower limit to 20–30 °C. The upper limit of the present Raman spectroscopic thermometer is 540 °C, which is derived from the bottoming out of Γ<sub>D1</sub>. This thermometer was applied to chondrites whose PMT are unknown. The obtained temperature values were consistent with the order of petrological type."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410282681522569473","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000312721900"}],"foaf:name":[{"@language":"en","@value":"HOMMA Yoshitaka"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Geochemical Research Center, Graduate School of Science, The University of 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Hikaru"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Department of Earth and Space Science, Graduate School of Science, Osaka University"}]}],"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":"2015","prism:volume":"110","prism:number":"6","prism:startingPage":"276","prism:endingPage":"282"},"reviewed":"false","url":[{"@id":"https://www.jstage.jst.go.jp/article/jmps/110/6/110_150713a/_pdf"}],"availableAt":"2015","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Raman%20spectroscopy","dc:title":"Raman spectroscopy"},{"@id":"https://cir.nii.ac.jp/all?q=Chondrites","dc:title":"Chondrites"},{"@id":"https://cir.nii.ac.jp/all?q=Carbonaceous%20material","dc:title":"Carbonaceous material"},{"@id":"https://cir.nii.ac.jp/all?q=Thermal%20history","dc:title":"Thermal history"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781845013120","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15K05339"},{"@type":"JGN","@value":"JP15K05339"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15K05339/"}],"notation":[{"@language":"ja","@value":"エッジワース・カイパーベルト天体起源岩片の探索によるニースモデルの物質科学的検証"},{"@language":"en","@value":"Verification of the Nice model by the search for Edgeworth-Kuiper belt objects in brecciated meteorites"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050022708917700864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"An automatic peak 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