Nanopublications

@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/RAajuutLjjJFTkWjFPSdo1U5F96u4NkyrI1pYmlUoMl9s/> .
@prefix this: <https://w3id.org/sciencelive/np/RAajuutLjjJFTkWjFPSdo1U5F96u4NkyrI1pYmlUoMl9s> .
@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/Contourite%20drifts%20in%20the%20Kai%20Formation%20on%20the%20mid-Norwegian%20margin%20commenced%20in%20the%20mid-Miocene%20%28slightly%20before%2011%20Ma%29.> cito:obtainsSupportFrom <https://doi.org/10.1016/j.margeo.2022.106974> , <https://doi.org/10.18710/DWOUPL> ;
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 "2026-03-13T14:01:27.000Z"^^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/Contourite%20drifts%20in%20the%20Kai%20Formation%20on%20the%20mid-Norwegian%20margin%20commenced%20in%20the%20mid-Miocene%20%28slightly%20before%2011%20Ma%29.> ;
    npx:wasCreatedAt <https://platform.sciencelive4all.org> ;
    rdfs:label "AIDA sentence: Contourite drifts in the Kai Formation on the mid-Norwegian margin commenced in the mid-Miocene (slightly before 11 Ma)." ;
    nt:wasCreatedFromTemplate <https://w3id.org/np/RALmXhDw3rHcMveTgbv8VtWxijUHwnSqhCmtJFIPKWVaA> .
  sub:sig npx:hasAlgorithm "RSA" ;
    npx:hasPublicKey "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" ;
    npx:hasSignature "FMUIVQXpBTeKjTYVShLVgrYaxTqkBWuni1/KNuT5POyGKkF3SAtNvlHjGdOrXoy1N4ORWgmpodJRCFDINteBgUq7+KFG8LiZl8c5RWplyoEz2Q/OV5ao8VsWfz96j/Kvz7fnvsxftBS3glXNGXONRoPjm3uEdYDFvsqUPTIsMp0gEpdcTWizMTaO+V1DRIT7Xczw96Ly24ibYXLScpHQb89qNp4dWILNEfBsmOICNsFRZAP3VfUzIe1SUHMLFYNjWSTya2pRR7M/OZ7z3sXWtegCnUg5daRwc4c0PSUZnt7Nueieodwwtpr/jLjEJmCshvz2qYcTqlQuK6ZlFDiroxZeLmVqV2Sq0g5pCOeZ1+qywGibpPptbnc2SciTjthmcTXGNQAidkPdQP0a2nJXetbpvXAMKGK/QzcCVr6NKmx8jE68tYvPChHOhJUrREgETI0G+uiu+UcCaUxicCx/n9zU6uYHle93BPXQ+ZyQVFt7NMBj6swK5XhJ11xJp/rdE0l7S5odc1ILWsjALnk0HuowhKAM13g3Rg9DT69o3iprfMCN/lV/Uou7jkQHhcPNEdgsCswa6tsnST8ikPTNy+nY1RNlvfqwupTWRbFCKddanmbdpcTz9Xd9T/EnU5mBtXGjZXe+Iayb8R2JgO5s5AXYRXm/tRA9Nrm7heFFqsg=" ;
    npx:hasSignatureTarget this: ;
    npx:signedBy <https://w3id.org/np/RALe_3U-0OKr-rc5FzaSc7xw1nPuGq1LkWoncmx6DXAV4/ai-mistral-ji> .
}