{"@context":{"ns0":"https://service.poleterresolide.fr/voc/variable/","rdf":"http://www.w3.org/1999/02/22-rdf-syntax-ns#","ns1":"http://www.w3.org/ns/sosa/","skos":"http://www.w3.org/2004/02/skos/core#","owl":"http://www.w3.org/2002/07/owl#","ns2":"https://terra-vocabulary.org/ncl/DataTerraRepositoryFairIncubator/motsClefs/","dct":"http://purl.org/dc/terms/","metadata_def":"http://data.bioontology.org/metadata/def/","ns3":"https://service.poleterresolide.fr/voc/"},"@graph":[{"@id":"ns0:c_a64d2bbc","@type":["ns1:ObservableProperty","skos:Concept","owl:NamedIndividual"],"owl:sameAs":{"@id":"ns2:c_6a64fce5"},"dct:source":{"@language":"fr","@value":"epos"},"skos:prefLabel":[{"@language":"fr","@value":"Temps d'arrivée"},{"@language":"en","@value":"arrival time"}],"dct:description":[{"@language":"fr","@value":"Le temps où une phase particulière d'onde arrive à un détecteur."},{"@language":"en","@value":"The time of the first onset of a seismic wave (e.g., P wave) as recorded by a seismograph. Arrival times are the basic data for locating earthquake hypocenters and for determining seismic velocity structures of the Earth"}],"metadata_def:mappingLoom":"tempsdarrive","metadata_def:mappingSameURI":{"@id":"ns0:c_a64d2bbc"},"skos:exactMatch":{"@id":"ns2:c_6a64fce5"},"skos:inScheme":{"@id":"ns3:variable"},"skos:topConceptOf":{"@id":"ns3:variable"}},{"@id":"ns0:skosCollection_4bee271e","skos:member":{"@id":"ns0:c_a64d2bbc"}}]}