{"@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/1362262943563763712.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.1122659"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.1122659"}}],"dc:title":[{"@value":"Global Mineralogical and Aqueous Mars History Derived from OMEGA/Mars Express Data"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Global mineralogical mapping of Mars by the Observatoire pour la Mineralogie, l'Eau, les Glaces et l'Activité (OMEGA) instrument on the European Space Agency's Mars Express spacecraft provides new information on Mars' geological and climatic history. Phyllosilicates formed by aqueous alteration very early in the planet's history (the “phyllocian” era) are found in the oldest terrains; sulfates were formed in a second era (the “theiikian” era) in an acidic environment. Beginning about 3.5 billion years ago, the last era (the “siderikian”) is dominated by the formation of anhydrous ferric oxides in a slow superficial weathering, without liquid water playing a major role across the planet.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382262943563763586","@type":"Researcher","foaf:name":[{"@value":"Jean-Pierre Bibring"}],"jpcoar:affiliationName":[{"@value":"Institut d'Astrophysique Spatiale (IAS), Bâtiment 121, 91405 Orsay Campus, France."},{"@value":"Department of Geological Sciences, Brown University, Providence, RI 02912, USA."},{"@value":"Department of Earth and Planetary Sciences, Washington University, St. Louis, MO 63130, USA."},{"@value":"Interactions et Dynamique des Environnement de Surface (IDES), Bâtiment 509, 91405 Orsay Campus, France."},{"@value":"Observatoire Midi-Pyrénées, Toulouse, France."}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943563763847","@type":"Researcher","foaf:name":[{"@value":"Yves Langevin"}],"jpcoar:affiliationName":[{"@value":"Institut d'Astrophysique Spatiale (IAS), Bâtiment 121, 91405 Orsay Campus, France."},{"@value":"Department of Geological Sciences, Brown University, Providence, RI 02912, USA."},{"@value":"Department of Earth and Planetary Sciences, Washington University, St. Louis, MO 63130, USA."},{"@value":"Interactions et Dynamique des Environnement de Surface (IDES), Bâtiment 509, 91405 Orsay Campus, France."},{"@value":"Observatoire Midi-Pyrénées, Toulouse, France."}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943563763840","@type":"Researcher","foaf:name":[{"@value":"John F. 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