@prefix dcat: <http://www.w3.org/ns/dcat#> .
@prefix dct: <http://purl.org/dc/terms/> .
@prefix foaf: <http://xmlns.com/foaf/0.1/> .
@prefix gsp: <http://www.opengis.net/ont/geosparql#> .
@prefix locn: <http://www.w3.org/ns/locn#> .
@prefix xsd: <http://www.w3.org/2001/XMLSchema#> .

<https://data.gov.au/dataset/90090a54-69ef-4990-8af0-ff4668d2f9fd> a dcat:Dataset ;
    dct:description "The Permian Yessabah Limestone, a thick crinoidal limestone unit, appears abruptly in the stratigraphic succession over a large area of the Hastings Block in northeastern New South Wales, disconformably overlying clastic rocks with sharply contrasting facies associations. The formation is part of a thick depositional sequence that began with a major sea-level fall at the end of the Carboniferous. The sea-level fall produced a major basinward shift in facies causing rejuvenation of streams and the deposition of braided-stream gravels in the onshore areas while a mass-movement association, the Parrabel Beds, was deposited offshore in the deep basin (the lowstand systems tract). The Yessabah Limestone was deposited as part of the transgressive systems tract in a shallow-marine high-energy environment as sea level again began to rise. The highstand systems tract then prograded over the Yessabah Limestone in the form of a distal turbidite association , the Warbro Formation and associated units, as sea level reached its maximum. The growth of both crinoids and bryozoa was prolific; their two distinctive faunal assemblages alternately dominated the sea floor, producing thick units of well-washed crinoid-rich limestone followed by a bryozoan-rich unit. As sea level rose, conditions became unsuitable for carbonate deposition and the area was again invaded by clastic sediments, forming a distal turbidite association that prograded across the limestones as part of the highstand systems tract." ;
    dct:identifier "90090a54-69ef-4990-8af0-ff4668d2f9fd" ;
    dct:issued "2026-03-25T17:49:29.486216"^^xsd:dateTime ;
    dct:language "eng" ;
    dct:modified "2026-03-25T17:49:29.486226"^^xsd:dateTime ;
    dct:publisher <https://data.gov.au/organization/91f054ec-d0c3-4d42-a89a-5daa2c7a6818> ;
    dct:spatial [ a dct:Location ;
            locn:geometry "POLYGON ((147.8900 -32.8700, 153.6900 -32.8700, 153.6900 -29.0300, 147.8900 -29.0300, 147.8900 -32.8700))"^^gsp:wktLiteral ] ;
    dct:title "Sequence analysis and depositional models of crinoidal limestones, Permian Yessabah Limestone, Manning-Macleay Basin, eastern Australia" ;
    dcat:distribution <https://data.gov.au/dataset/90090a54-69ef-4990-8af0-ff4668d2f9fd/resource/2080dfed-21ed-4bb7-b52d-7a8c7f067158>,
        <https://data.gov.au/dataset/90090a54-69ef-4990-8af0-ff4668d2f9fd/resource/3bd5580d-e9e9-4279-a12e-2d4ab458b9dc> ;
    dcat:keyword "Earth Sciences",
        "GA Publication",
        "Journal",
        "NSW",
        "Published_External" .

<https://data.gov.au/dataset/90090a54-69ef-4990-8af0-ff4668d2f9fd/resource/2080dfed-21ed-4bb7-b52d-7a8c7f067158> a dcat:Distribution ;
    dct:description "Journal article (pdf)" ;
    dct:format "PDF" ;
    dct:issued "2026-03-25T17:49:29.489044"^^xsd:dateTime ;
    dct:modified "2026-03-25T17:49:29.476100"^^xsd:dateTime ;
    dct:title "Journal article (pdf)" ;
    dcat:accessURL <https://d28rz98at9flks.cloudfront.net/81287/Jou1991_v12_n2_p145.pdf> .

<https://data.gov.au/dataset/90090a54-69ef-4990-8af0-ff4668d2f9fd/resource/3bd5580d-e9e9-4279-a12e-2d4ab458b9dc> a dcat:Distribution ;
    dct:format "HTML" ;
    dct:issued "2026-03-25T17:49:29.489052"^^xsd:dateTime ;
    dct:modified "2026-03-25T17:49:29.476218"^^xsd:dateTime ;
    dct:title "Unnamed resource" ;
    dcat:accessURL <http://www.abs.gov.au/ausstats/abs@.nsf/Latestproducts/1297.0Main%20Features32008?opendocument&tabname=Summary&prodno=1297.0&issue=2008&num=&view=> .

<https://data.gov.au/organization/91f054ec-d0c3-4d42-a89a-5daa2c7a6818> a foaf:Agent ;
    foaf:mbox "clientservices@ga.gov.au" ;
    foaf:name "Geoscience Australia Data" .