@prefix dcat: <http://www.w3.org/ns/dcat#> .
@prefix dct: <http://purl.org/dc/terms/> .
@prefix foaf: <http://xmlns.com/foaf/0.1/> .
@prefix vcard: <http://www.w3.org/2006/vcard/ns#> .
@prefix xsd: <http://www.w3.org/2001/XMLSchema#> .

<https://rec.harvest-normandie.data4citizen.com/dataset/oai-hal-hal-00023846v1> a dcat:Dataset ;
    dct:description """
              n the French Massif Central, the Rouergue–Albigeois area consists of three tectonic units stacked during the Hercynian orogeny. The structural analysis of the units and particularly the quartz left angle bracketcright-pointing angle bracket axis, textural and structural observations in the syntectonic Pinet-type plutons allow us to determine the deformation history. A first thrusting event, D1, is responsible for a southwestward emplacement of the high-grade Lévézou nappe, above the Lower Gneiss Unit itself overlying the para-autochthonous micaschists. In Late Devonian–Early Carboniferous, this stack of nappes experienced a second event, D2, characterized by a top-to-the-NW emplacement under medium pressure/medium temperature conditions of the para-autochtonous unit upon the Lower Gneiss Unit. During D2, the Pinet-type plutons were deformed by a shearing consistent with the kinematics recorded in the country rocks. In contrast to previous works, which considered the Pinet-type plutons emplacement to be coeval with the D2 event, we argue that the emplacement of the plutons occurred during the top-to-the-SW D1 nappe stacking. This work emphasizes the importance of the quartz left angle bracketcright-pointing angle bracket axis and microstructure analysis for the identification of the early structural history in polyphase deformed terranes.
            """ ;
    dct:identifier "hal-00023846" ;
    dct:issued "2026-05-25T22:02:15.383326"^^xsd:dateTime ;
    dct:language "en" ;
    dct:modified "2026-05-25T22:02:15.383331"^^xsd:dateTime ;
    dct:publisher <https://rec.harvest-normandie.data4citizen.com/organization/cce9db95-46d9-4dc2-84b6-764215d0a002> ;
    dct:title "Granitoid emplacement during a thrusting event: structural analysis, microstructuel and quartz-c-axis patterns. An example from hercynian plutons in the French Massif Central." ;
    dcat:contactPoint [ a vcard:Organization ;
            vcard:fn "CCSD" ] ;
    dcat:distribution <https://rec.harvest-normandie.data4citizen.com/dataset/oai-hal-hal-00023846v1/resource/2e34ec81-5e4d-42d9-99a3-4bd22219c029> ;
    dcat:keyword "granite-emplacement",
        "hercynian-belt",
        "infoeu-reposemanticsarticle",
        "journal-articles",
        "nappe-tectonics",
        "polyphase-deformation",
        "quartz-left-angle-bracketcright-pointing-angle-bracket-axis-fabrics",
        "sdustutesciences-of-the-universe-physicsearth-sciencestectonics" ;
    dcat:landingPage <ISSN:%200191-8141> .

<ISSN:%200191-8141> a foaf:Document .

<https://rec.harvest-normandie.data4citizen.com/dataset/oai-hal-hal-00023846v1/resource/2e34ec81-5e4d-42d9-99a3-4bd22219c029> a dcat:Distribution ;
    dct:format "HTML" ;
    dct:issued "2026-05-25T22:02:15.424187"^^xsd:dateTime ;
    dct:modified "2026-05-25T22:02:15.356309"^^xsd:dateTime ;
    dct:title "Granitoid emplacement during a thrusting event: structural analysis, microstructuel and quartz-c-axis patterns. An example from hercynian plutons in the French Massif Central." ;
    dcat:accessURL <https://insu.hal.science/hal-00023846> .

<https://rec.harvest-normandie.data4citizen.com/organization/cce9db95-46d9-4dc2-84b6-764215d0a002> a foaf:Agent ;
    foaf:name "test_moissonnage_selune" .