@prefix cito: <http://purl.org/spar/cito/> .
@prefix dcterms: <http://purl.org/dc/terms/> .
@prefix foaf: <http://xmlns.com/foaf/0.1/> .
@prefix hycl: <http://purl.org/petapico/o/hycl#> .
@prefix np: <http://www.nanopub.org/nschema#> .
@prefix npx: <http://purl.org/nanopub/x/> .
@prefix nt: <https://w3id.org/np/o/ntemplate/> .
@prefix prov: <http://www.w3.org/ns/prov#> .
@prefix rdfs: <http://www.w3.org/2000/01/rdf-schema#> .
@prefix sub: <https://w3id.org/sciencelive/np/RACmBfS1Jqgf-ieaZzsO7qWqTTf__lqGEPvbJUMFy9mJc/> .
@prefix this: <https://w3id.org/sciencelive/np/RACmBfS1Jqgf-ieaZzsO7qWqTTf__lqGEPvbJUMFy9mJc> .
@prefix xsd: <http://www.w3.org/2001/XMLSchema#> .

sub:Head {
  this: np:hasAssertion sub:assertion;
    np:hasProvenance sub:provenance;
    np:hasPublicationInfo sub:pubinfo;
    a np:Nanopublication .
}

sub:assertion {
  <http://purl.org/aida/Core%2028-03%20in%20the%20Norwegian%20Channel%20experienced%20simulated%20peak%20currents%20of%200.5%20m%2Fs%20during%20the%20Storegga%20tsunami%2C%20capable%20of%20stirring%20fine-grained%20sediments.>
    cito:obtainsSupportFrom <https://doi.org/10.1038/s41467-024-47347-9>, <https://doi.org/10.18710/6KDQ7I>;
    a hycl:AIDA-Sentence .
}

sub:provenance {
  sub:assertion prov:wasAttributedTo <https://w3id.org/np/RALe_3U-0OKr-rc5FzaSc7xw1nPuGq1LkWoncmx6DXAV4/ai-mistral-ji> .
}

sub:pubinfo {
  <https://w3id.org/np/RALe_3U-0OKr-rc5FzaSc7xw1nPuGq1LkWoncmx6DXAV4/ai-mistral-ji>
    foaf:name "ai-mistral-ji" .
  
  this: dcterms:created "2026-03-13T14:19:09.000Z"^^xsd:dateTime;
    dcterms:creator <https://w3id.org/np/RALe_3U-0OKr-rc5FzaSc7xw1nPuGq1LkWoncmx6DXAV4/ai-mistral-ji>;
    dcterms:license <https://creativecommons.org/licenses/by/4.0/>;
    npx:hasNanopubType hycl:AIDA-Sentence, <http://purl.org/petapico/o/hycl>;
    npx:introduces <http://purl.org/aida/Core%2028-03%20in%20the%20Norwegian%20Channel%20experienced%20simulated%20peak%20currents%20of%200.5%20m%2Fs%20during%20the%20Storegga%20tsunami%2C%20capable%20of%20stirring%20fine-grained%20sediments.>;
    npx:wasCreatedAt <https://platform.sciencelive4all.org>;
    rdfs:label "AIDA sentence: Core 28-03 in the Norwegian Channel experienced simulated peak currents of 0.5 m/s during the Storegga tsunami, capable of stirring fine-grained sediments.";
    nt:wasCreatedFromTemplate <https://w3id.org/np/RALmXhDw3rHcMveTgbv8VtWxijUHwnSqhCmtJFIPKWVaA> .
  
  sub:sig npx:hasAlgorithm "RSA";
    npx:hasPublicKey "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";
    npx:hasSignature "nJ9hq/RrO0cuiPJrjid5EktcJ7Hu4OEm+x/D1adJ6S1KgwUGpm1t2rUURpq7OnFOm3KhTn+0cTVFfuDzpfjSQ0jdkQxhaVQrP2+m7+Uwv9kkBvcRIrXFkvA0pN/JFgvYOhmHoV5/0TwJr1GGgfgafxKNjK7sR8nQHrW3yk+N30f5ZR+rnGCE+jxXWXtQnNb2sKqHtIL5Xe1Yg2/PfeDPHfbMpcEA63pDUrkSLvqCuUNOMpgeLsu3DefEYVNpqon36is+kb18pJgTdCg9vdt6HoY6mi/dOD09e02DMrTV7zEuXEVYgxpLWEAtVjoggJBbQoLCt1peN1VtPFBjR376sylhiJDQaB1q3AwUHfI0TAo4K4tjC0JLHbnmG7epbijUpUl4ZBoo0CTe/5BzxiCRAEK4zPDi10ImFBrrlGXlcEfcLTrjXbi6J4/oOSF/jQouYQreaNO7MmvJTZnHchn/CzZJdj91yuWhu1CfDu+hjx2l+WJZejp9Kd3cC5nZuHsWJ2CYbMrLl3X5EPZJ9aDQu4JH3JSHv0t7hJ1y7hniF8Il5oCeGXHN2tzGXEnkLCApAX6H9O3Fun9jc7kgsOlmtCmVVppG2dRfWC+TswwMR1eQiE2wVu4F1GxWiWQf3TVK+QMkuaB92vOM3EPwtB3jfWn6Brnh1R82GDXo2ZJk0l0=";
    npx:hasSignatureTarget this:;
    npx:signedBy <https://w3id.org/np/RALe_3U-0OKr-rc5FzaSc7xw1nPuGq1LkWoncmx6DXAV4/ai-mistral-ji> .
}