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/RAYZEQkE7wxD2RRKxdZrK6xlu-lrbN19IH7Llt2gH817A/> .
@prefix this: <https://w3id.org/sciencelive/np/RAYZEQkE7wxD2RRKxdZrK6xlu-lrbN19IH7Llt2gH817A> .
@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/Along-slope%20bottom%20current%20deposits%20%28contourites%29%20are%20volumetrically%20more%20significant%20on%20the%20mid-Norwegian%20margin%20compared%20to%20down-slope%20glacial%20deposits%20during%20the%20Neogene.> 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" .
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    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/Along-slope%20bottom%20current%20deposits%20%28contourites%29%20are%20volumetrically%20more%20significant%20on%20the%20mid-Norwegian%20margin%20compared%20to%20down-slope%20glacial%20deposits%20during%20the%20Neogene.> ;
    npx:wasCreatedAt <https://platform.sciencelive4all.org> ;
    rdfs:label "AIDA sentence: Along-slope bottom current deposits (contourites) are volumetrically more significant on the mid-Norwegian margin compared to down-slope glacial deposits during the Neogene." ;
    nt:wasCreatedFromTemplate <https://w3id.org/np/RALmXhDw3rHcMveTgbv8VtWxijUHwnSqhCmtJFIPKWVaA> .
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    npx:hasSignatureTarget this: ;
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