{"@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/1362825895437161472.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2010je003716"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2010JE003716"}},{"identifier":{"@type":"URI","@value":"http://www.agu.org/journals/je/je1102/2010JE003716/2010JE003716.pdf"}}],"dc:title":[{"@value":"Global surface slopes and roughness of the Moon from the Lunar Orbiter Laser Altimeter"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380017282213931393","@type":"Researcher","foaf:name":[{"@value":"M. A. Rosenburg"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895437161344","@type":"Researcher","foaf:name":[{"@value":"O. Aharonson"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895437161477","@type":"Researcher","foaf:name":[{"@value":"J. W. Head"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895437161474","@type":"Researcher","foaf:name":[{"@value":"M. A. Kreslavsky"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895437161476","@type":"Researcher","foaf:name":[{"@value":"E. Mazarico"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895437161472","@type":"Researcher","foaf:name":[{"@value":"G. A. Neumann"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895437161473","@type":"Researcher","foaf:name":[{"@value":"D. E. Smith"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895437161345","@type":"Researcher","foaf:name":[{"@value":"M. H. Torrence"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895437161478","@type":"Researcher","foaf:name":[{"@value":"M. T. Zuber"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2011-02-03","prism:volume":"116","prism:number":"E2","prism:startingPage":"E02001"},"reviewed":"false","dc:rights":["http://doi.wiley.com/10.1002/tdm_license_1.1"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2010JE003716"},{"@id":"http://www.agu.org/journals/je/je1102/2010JE003716/2010JE003716.pdf"}],"createdAt":"2011-02-02","modifiedAt":"2021-07-21","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004232184363264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Constraint on subsurface structures beneath Reiner Gamma on the Moon using the Kaguya Lunar Radar Sounder"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285709358677632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"<i>FERMI</i>OBSERVATIONS OF γ-RAY EMISSION FROM THE MOON"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285710774631424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Is the Linné impact crater morphology influenced by the rheological layering on the Moon's surface? Insights from numerical modeling"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179753998208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Variation of the lunar highland surface roughness at baseline 0.15–100 km and the relationship to relative age"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588380582470784","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Ganymede Laser Altimeter (GALA) on the Jupiter Icy moons Explorer (JUICE) Mission"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567354653312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Leg-circle transformable wheel for improved runnability of a lunar rover"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763101316864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Science Objectives of the Ganymede Laser Altimeter (GALA) for the JUICE Mission"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792015351552","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Utilization of a meteorological satellite as a space telescope : the lunar mid-infrared spectrum as seen by Himawari-8"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2010je003716"},{"@type":"CROSSREF","@value":"10.1016/j.icarus.2015.03.020_references_DOI_L2DOwbTSYNDsgsRQDi9k2eIJSBT"},{"@type":"CROSSREF","@value":"10.1186/s40623-022-01662-x_references_DOI_L2DOwbTSYNDsgsRQDi9k2eIJSBT"},{"@type":"CROSSREF","@value":"10.1088/0004-637x/758/2/140_references_DOI_L2DOwbTSYNDsgsRQDi9k2eIJSBT"},{"@type":"CROSSREF","@value":"10.1111/maps.12892_references_DOI_L2DOwbTSYNDsgsRQDi9k2eIJSBT"},{"@type":"CROSSREF","@value":"10.1002/2013gl059091_references_DOI_L2DOwbTSYNDsgsRQDi9k2eIJSBT"},{"@type":"CROSSREF","@value":"10.1007/s11214-025-01149-7_references_DOI_L2DOwbTSYNDsgsRQDi9k2eIJSBT"},{"@type":"CROSSREF","@value":"10.1177/1045389x20952545_references_DOI_L2DOwbTSYNDsgsRQDi9k2eIJSBT"},{"@type":"CROSSREF","@value":"10.2322/tastj.17.234_references_DOI_L2DOwbTSYNDsgsRQDi9k2eIJSBT"}]}