{"@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/1360011142933825536.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1073/pnas.1116236109"}},{"identifier":{"@type":"URI","@value":"https://pnas.org/doi/pdf/10.1073/pnas.1116236109"}},{"identifier":{"@type":"PMID","@value":"22371561"}}],"dc:title":[{"@value":"Space environment of an asteroid preserved on micrograins returned by the Hayabusa spacecraft"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>\n            Records of micrometeorite collisions at down to submicron scales were discovered on dust grains recovered from near-Earth asteroid 25143 (Itokawa). Because the grains were sampled from very near the surface of the asteroid, by the Hayabusa spacecraft, their surfaces reflect the low-gravity space environment influencing the physical nature of the asteroid exterior. The space environment was examined by description of grain surfaces and asteroidal scenes were reconstructed. Chemical and O isotope compositions of five lithic grains, with diameters near 50 μm, indicate that the uppermost layer of the rubble-pile-textured Itokawa is largely composed of equilibrated LL-ordinary-chondrite-like material with superimposed effects of collisions. The surfaces of the grains are dominated by fractures, and the fracture planes contain not only sub-μm-sized craters but also a large number of sub-μm- to several-μm-sized adhered particles, some of the latter composed of glass. The size distribution and chemical compositions of the adhered particles, together with the occurrences of the sub-μm-sized craters, suggest formation by hypervelocity collisions of micrometeorites at down to nm scales, a process expected in the physically hostile environment at an asteroid’s surface. We describe impact-related phenomena, ranging in scale from 10\n            <jats:sup>-9</jats:sup>\n            to 10\n            <jats:sup>4</jats:sup>\n            meters, demonstrating the central role played by impact processes in the long-term evolution of planetary bodies. Impact appears to be an important process shaping the exteriors of not only large planetary bodies, such as the moon, but also low-gravity bodies such as asteroids.\n          </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380298342070316556","@type":"Researcher","foaf:name":[{"@value":"Eizo Nakamura"}],"jpcoar:affiliationName":[{"@value":"The Pheasant Memorial Laboratory for Geochemistry and Cosmochemistry, Institute for Study of the Earth’s Interior, Okayama University, Misasa, Tottori 682-0193, Japan; and"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298342070316558","@type":"Researcher","foaf:name":[{"@value":"Akio Makishima"}],"jpcoar:affiliationName":[{"@value":"The Pheasant Memorial Laboratory for Geochemistry and Cosmochemistry, Institute for Study of the Earth’s Interior, Okayama University, Misasa, Tottori 682-0193, Japan; and"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298342070316545","@type":"Researcher","foaf:name":[{"@value":"Takuya Moriguti"}],"jpcoar:affiliationName":[{"@value":"The Pheasant Memorial Laboratory for Geochemistry and Cosmochemistry, Institute for Study of the Earth’s Interior, Okayama University, Misasa, Tottori 682-0193, Japan; and"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298342070316557","@type":"Researcher","foaf:name":[{"@value":"Katsura Kobayashi"}],"jpcoar:affiliationName":[{"@value":"The Pheasant Memorial Laboratory for Geochemistry and Cosmochemistry, Institute for Study of the Earth’s Interior, Okayama University, Misasa, Tottori 682-0193, Japan; and"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298342070316546","@type":"Researcher","foaf:name":[{"@value":"Ryoji Tanaka"}],"jpcoar:affiliationName":[{"@value":"The Pheasant Memorial Laboratory for Geochemistry and Cosmochemistry, Institute for Study of the Earth’s Interior, Okayama University, Misasa, Tottori 682-0193, Japan; and"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298342070316559","@type":"Researcher","foaf:name":[{"@value":"Tak Kunihiro"}],"jpcoar:affiliationName":[{"@value":"The Pheasant Memorial Laboratory for Geochemistry and Cosmochemistry, Institute for Study of the Earth’s Interior, Okayama University, Misasa, Tottori 682-0193, Japan; and"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298342070316552","@type":"Researcher","foaf:name":[{"@value":"Tatsuki Tsujimori"}],"jpcoar:affiliationName":[{"@value":"The Pheasant Memorial Laboratory for Geochemistry and Cosmochemistry, Institute for Study of the Earth’s Interior, Okayama University, Misasa, Tottori 682-0193, Japan; and"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298342070316550","@type":"Researcher","foaf:name":[{"@value":"Chie Sakaguchi"}],"jpcoar:affiliationName":[{"@value":"The Pheasant Memorial Laboratory for Geochemistry and Cosmochemistry, Institute for Study of the Earth’s Interior, Okayama University, Misasa, Tottori 682-0193, Japan; and"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298342070316553","@type":"Researcher","foaf:name":[{"@value":"Hiroshi Kitagawa"}],"jpcoar:affiliationName":[{"@value":"The Pheasant Memorial Laboratory for Geochemistry and Cosmochemistry, Institute for Study of the Earth’s Interior, Okayama University, Misasa, Tottori 682-0193, Japan; and"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298342070316551","@type":"Researcher","foaf:name":[{"@value":"Tsutomu Ota"}],"jpcoar:affiliationName":[{"@value":"The Pheasant Memorial Laboratory for Geochemistry and Cosmochemistry, Institute for Study of the Earth’s Interior, Okayama University, Misasa, Tottori 682-0193, Japan; and"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298342070316555","@type":"Researcher","foaf:name":[{"@value":"Yusuke Yachi"}],"jpcoar:affiliationName":[{"@value":"The Pheasant Memorial Laboratory for Geochemistry and Cosmochemistry, Institute for Study of the Earth’s Interior, Okayama University, Misasa, Tottori 682-0193, Japan; and"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298342070316561","@type":"Researcher","foaf:name":[{"@value":"Toru Yada"}],"jpcoar:affiliationName":[{"@value":"Japan Aerospace Exploration Agency, Yoshinodai 3-1-1, Chuo, Sagamihara, Kanagawa 252-5210, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298342070316544","@type":"Researcher","foaf:name":[{"@value":"Masanao Abe"}],"jpcoar:affiliationName":[{"@value":"Japan Aerospace Exploration Agency, Yoshinodai 3-1-1, Chuo, Sagamihara, Kanagawa 252-5210, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298342070316547","@type":"Researcher","foaf:name":[{"@value":"Akio Fujimura"}],"jpcoar:affiliationName":[{"@value":"Japan Aerospace Exploration Agency, Yoshinodai 3-1-1, Chuo, Sagamihara, Kanagawa 252-5210, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298342070316549","@type":"Researcher","foaf:name":[{"@value":"Munetaka Ueno"}],"jpcoar:affiliationName":[{"@value":"Japan Aerospace Exploration Agency, Yoshinodai 3-1-1, Chuo, Sagamihara, Kanagawa 252-5210, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298342070316548","@type":"Researcher","foaf:name":[{"@value":"Toshifumi Mukai"}],"jpcoar:affiliationName":[{"@value":"Japan Aerospace Exploration Agency, Yoshinodai 3-1-1, Chuo, Sagamihara, Kanagawa 252-5210, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298342070316560","@type":"Researcher","foaf:name":[{"@value":"Makoto Yoshikawa"}],"jpcoar:affiliationName":[{"@value":"Japan Aerospace Exploration Agency, Yoshinodai 3-1-1, Chuo, Sagamihara, Kanagawa 252-5210, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298342070316554","@type":"Researcher","foaf:name":[{"@value":"Jun’ichiro Kawaguchi"}],"jpcoar:affiliationName":[{"@value":"Japan Aerospace Exploration Agency, Yoshinodai 3-1-1, Chuo, Sagamihara, Kanagawa 252-5210, Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00278424"},{"@type":"EISSN","@value":"10916490"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/00278424"}],"prism:publicationName":[{"@value":"Proceedings of the National Academy of Sciences"}],"dc:publisher":[{"@value":"Proceedings of the National Academy of Sciences"}],"prism:publicationDate":"2012-02-27","prism:volume":"109","prism:number":"11","prism:startingPage":"E624"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"https://pnas.org/doi/pdf/10.1073/pnas.1116236109"}],"createdAt":"2012-02-28","modifiedAt":"2022-04-13","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001335810696960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Three-dimensional microstructure of samples recovered from asteroid 25143 Itokawa: Comparison with LL5 and LL6 chondrite particles"},{"@value":"Three‐dimensional microstructure of samples recovered from asteroid 25143 Itokawa: Comparison with <scp>LL</scp>5 and <scp>LL</scp>6 chondrite particles"},{"@value":"Three‐dimensional microstructure of samples recovered from asteroid 25143 Itokawa: Comparison with LL5 and LL6 chondrite particles"}]},{"@id":"https://cir.nii.ac.jp/crid/1050022089736834560","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"H, C, and N isotopic compositions of Hayabusa category 3 organic samples"}]},{"@id":"https://cir.nii.ac.jp/crid/1050282810809484928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Mineralogy and noble gas isotopes of micrometeorites collected from Antarctic snow Planetary Science"},{"@value":"Mineralogy and noble gas isotopes of micrometeorites collected from Antarctic snow"}]},{"@id":"https://cir.nii.ac.jp/crid/1050287628878668032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Albedo of Ryugu: Evidence for a High Organic Abundance, as Inferred from the Hayabusa2 Touchdown Maneuver"}]},{"@id":"https://cir.nii.ac.jp/crid/1050296575288226560","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A history of mild shocks experienced by the regolith particles on hydrated asteroid Ryugu"}]},{"@id":"https://cir.nii.ac.jp/crid/1050587981430430464","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Population characteristics of submicrometer-sized craters on regolith particles from asteroid Itokawa"}]},{"@id":"https://cir.nii.ac.jp/crid/1050845763736009600","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Hayabusa2 Mission Overview"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232135320704","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Oxygen three-isotope ratios of silicate particles returned from asteroid Itokawa by the Hayabusa spacecraft: A strong link with equilibrated LL chondrites"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232184459648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Increase in cratering efficiency with target curvature in strength-controlled craters"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233487076864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Circa 1 Ga sub-seafloor hydrothermal alteration imprinted on the Horoman peridotite massif"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233853507456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Magnetic Sampler for Regolith Particles on Asteroids"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004235797783680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sylvite and halite on particles recovered from 25143 Itokawa: A preliminary report"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004235797884544","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Boron abundances and isotopic ratios of olivine grains on Itokawa returned by the Hayabusa spacecraft"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009581503733120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Preliminary analysis of the Hayabusa2 samples returned from C-type asteroid Ryugu"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283690409123840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Hayabusa2 Sampler: Collection of Asteroidal Surface Material"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707161031936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Space weathering of silicate regoliths with various FeO contents: New insights from laser irradiation experiments and theoretical spectral simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643773574528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Magmatic-hydrothermal processes of the Laojunshan metamorphic massif in Southeastern Asia: Evidence from chemical and B-isotopic variations of deformed tourmalines"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298345571340800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Hayabusa2 Sample Catcher and Container: Metal-Seal System for Vacuum Encapsulation of Returned Samples with Volatiles and Organic Compounds Recovered from C-Type Asteroid Ryugu"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565168299709440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Hayabusa‐returned sample curation in the Planetary Material Sample Curation Facility of JAXA"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567181389222272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dust Phenomena Relating to Airless Bodies"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182137789440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Surface and internal structures of a space-weathered rim of an Itokawa regolith particle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567185751049472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Space weathered rims found on the surfaces of the Itokawa dust particles"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567185751202944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Investigation of cutting methods for small samples of Hayabusa and future sample return missions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092661204480","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Combining IR and X‐ray microtomography data sets: Application to Itokawa particles and to Paris meteorite"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657096825216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Nanomorphology of Itokawa regolith particles: Application to space-weathering processes affecting the Itokawa asteroid"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593728154880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The trace element composition of chondrule constituents: Implications for sample return methodologies and the chondrule silicate reservoir"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861295375314688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Site selection for the Hayabusa2 artificial cratering and subsurface material sampling on Ryugu"}]},{"@id":"https://cir.nii.ac.jp/crid/1360862720847033472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A curation for uncontaminated Hayabusa2-returned samples in the extraterrestrial curation center of JAXA: from the beginning to present day"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865814734801408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Microstructural and chemical features of impact melts on Ryugu particle surfaces: Records of interplanetary dust hit on asteroid Ryugu"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206526497408","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"High-pressure polymorphs in shocked meteorites"},{"@language":"ja","@value":"衝撃を経験した隕石に含まれる高圧相"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679531397888","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Hayabusa2: Scientific importance of samples returned from C-type near-Earth asteroid (162173) 1999 JU<sub>3</sub>"},{"@value":"Hayabusa2 : Scientific importance of samples returned from C-type near-Earth asteroid (162173) 1999 JU₃"},{"@value":"Hayabusa2: Scientific importance of samples returned from near-Earth C-type asteroid 1999 JU3"},{"@value":"Hayabusa2: scientific importance of samples 1027 returned from C-type near-Earth asteroid (162173) 1999 JU3"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238083288576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Hypervelocity collision and water-rock interaction in space preserved in the Chelyabinsk ordinary chondrite"}]},{"@id":"https://cir.nii.ac.jp/crid/1390855300947540480","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"On the origin and evolution of the asteroid Ryugu: A comprehensive geochemical perspective"}]},{"@id":"https://cir.nii.ac.jp/crid/1521699230566496768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Low-Resolution Spectrum of the Zodiacal Light with the AKARI InfraRed Camera"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870366937454976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Special issue \"science of solar system materials examined from Hayabusa and future missions (II)\""}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842057867776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Analytical protocols for Phobos regolith samples returned by the Martian Moons eXploration (MMX) mission"}]},{"@id":"https://cir.nii.ac.jp/crid/2120589364339957504","@type":"OtherWorks","resourceType":"学術雑誌論文(journal article)","relationType":["isIdenticalTo"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Space environment of an asteroid preserved on micrograins returned by the Hayabusa spacecraft"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1073/pnas.1116236109"},{"@type":"OPENAIRE","@value":"doi_dedup___::a21f16e081e6f3ae14423ea6e8f073df"},{"@type":"IRDB","@value":"oai:irdb.nii.ac.jp:01332:0004474325_isIdenticalTo_DOI_E7TU3sHasKov3w8R415OSqEPj56"},{"@type":"CROSSREF","@value":"10.1111/maps.12177_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1038/s41598-018-28219-x_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1111/maps.12333_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1111/maps.12686_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2016.05.011_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1016/j.icarus.2014.03.021_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-91_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1038/s41550-021-01550-6_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1016/j.pss.2022.105519_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1038/s41550-023-01947-5_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1007/s11214-017-0338-8_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1007/s11214-017-0377-1_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1093/pasj/65.6.119_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.2343/geochemj.2.0350_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1016/j.icarus.2017.12.017_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1016/j.lithos.2022.106609_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.2183/pjab.98.015_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1111/maps.12027_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1007/s11214-018-0527-0_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1111/maps.12111_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1111/maps.12322_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.2183/pjab.95.013_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1111/maps.13538_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1089/ast.2019.2198_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01438-9_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1186/s40623-023-01924-2_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1007/s11214-016-0289-5_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1186/s40623-015-0261-8_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0617-3_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1016/j.icarus.2017.10.019_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2013.08.009_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.2465/gkk.131120_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1061/(asce)as.1943-5525.0000797_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1111/maps.13665_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1126/sciadv.adi7203_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"},{"@type":"CROSSREF","@value":"10.1016/j.icarus.2015.05.001_references_DOI_UlksU3yoNeT06pnrrktHoUfZMYk"}]}