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<div id="pylode">made by <a href="http://github.com/rdflib/pyLODE">
<span style="color:#329545;">p</span><span style="color:#f9cb33;">y</span>LODE</a>
<span style="font-size:smaller;">2.8.6</span>
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<h1>Geologic Features Ontology</h1>
<section id="metadata">
<h2 style="display:none;">Metadata</h2>
<dl>
<dt>URI</dt>
<dd><code>https://linked.data.gov.au/def/geofeatures</code></dd>
<dt><a class="proplink" href="https://www.dublincore.org/specifications/dublin-core/dcmi-terms/#http://purl.org/dc/terms/publisher">Publisher</a>(s)</dt>
<dd>
<a href="https://linked.data.gov.au/org/gsq">Geological Survey of Queensland</a>
(<a href="mailto:[email protected]">[email protected]</a>)<br/>
</dd>
<dt><a class="proplink" href="https://www.dublincore.org/specifications/dublin-core/dcmi-terms/#http://purl.org/dc/terms/creator">Creator</a>(s)</dt>
<dd>
<a href="https://orcid.org/0000-0001-5489-9590">John L. McKellar</a>
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(<a href="mailto:[email protected]">[email protected]</a>) of
<a href="https://www.business.qld.gov.au/industries/mining-energy-water/resources/geoscience-information/gsq">Geological Survey of Queensland</a><br/>
<a href="https://orcid.org/0000-0002-8742-7730">Nicholas J. Car</a>
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(<a href="mailto:[email protected]">[email protected]</a>) of
<a href="https://surroundaustralia.com">SURROUND Australia Pty Ltd</a><br/>
</dd>
<dt><a class="proplink" href="https://www.dublincore.org/specifications/dublin-core/dcmi-terms/#http://purl.org/dc/terms/contributor">Contributor</a>(s)</dt>
<dd>
<a href="https://linked.data.gov.au/org/gsq">Geological Survey of Queensland</a>
(<a href="mailto:[email protected]">[email protected]</a>)<br/>
Derek Hoy
(<a href="mailto:[email protected]">[email protected]</a>) of
<a href="https://www.business.qld.gov.au/industries/mining-energy-water/resources/geoscience-information/gsq">Geological Survey of Queensland</a><br/>
</dd>
<dt><a class="proplink" href="https://www.dublincore.org/specifications/dublin-core/dcmi-terms/#http://purl.org/dc/terms/created">Created</a></dt>
<dd>2020-01-23</dd>
<dt><a class="proplink" href="https://www.dublincore.org/specifications/dublin-core/dcmi-terms/#http://purl.org/dc/terms/modified">Modified</a></dt>
<dd>2020-03-10</dd>
<dt>Version Information</dt>
<dd>Most ontology content but not complete diagrammatic coverage.</dd>
<dt>Version URI</dt>
<dd><a href="https://linked.data.gov.au/def/geofeatures/0.5">geof:0.5</a></dd>
<dt>Imports</dt>
<dd>
<a href="http://www.opengis.net/ont/geosparql">http://www.opengis.net/ont/geosparql</a><br/>
<a href="http://www.w3.org/2004/02/skos/core">http://www.w3.org/2004/02/skos/core</a><br/>
</dd>
<dt>Ontology RDF</dt>
<dd><a href="geofeatures.ttl">RDF (turtle)</a></dd>
<dt>Code Repository</dt>
<dd><a href="https://github.com/geological-survey-of-queensland/geofeatures-ont">https://github.com/geological-survey-of-queensland/geofeatures-ont</a></dd>
</dl>
<h2>Description</h2>
<div id="description">
<p>This OWL ontology describes classes of geologic/geological feature relevant to the duties of the Geological Survey of Queensland.</p>
<p>Elements of this ontology are designed to fit within other, broader, ontologies, in particular <a href="https://github.com/ESIPFed/sweet">Semantic Web for Earth and Environmental Terminology (SWEET) Ontologies</a> ontologies. </p>
<p>The core of this ontology is a class hierarchy starting with "geologic province", as it is defined in SWEET, and extending down into multiple subclasses of it.</p>
</div>
</section>
<section id="toc">
<h2>Table of Contents</h2>
<ol>
<li><a href="#classes">Classes</a></li>
<li><a href="#namespaces">Namespaces</a></li>
<li><a href="#legend">Legend</a></li>
</ol>
</section>
<!--
<section id="overview">
<h2>Overview</h2>
<div class="figure">
<div style="width:500px; height:50px; background-color: lightgrey; border:solid 2px grey; padding:10px;margin-bottom:5px; text-align:center;">Pictures say 1,000 words</div>
<div class="caption"><strong>Figure 1:</strong> Ontology overview</div>
</div>
</section>
-->
<section id="classes">
<h2>Classes <span style="float:right; font-size:smaller;"><a href="">↑</a></span></h2>
<ul class="hlist">
<li><a href="#abundancezone">abundance zone</a></li>
<li><a href="#ancientcontinent">ancient continent</a></li>
<li><a href="#anticline">anticline</a></li>
<li><a href="#anticlinorium">anticlinorium</a></li>
<li><a href="#antiform">antiform</a></li>
<li><a href="#antiformalstack">antiformal stack</a></li>
<li><a href="#arch">arch</a></li>
<li><a href="#assemblagezone">assemblage zone</a></li>
<li><a href="#associationzone">association zone</a></li>
<li><a href="#bed">bed</a></li>
<li><a href="#beds">beds</a></li>
<li><a href="#biostratigraphicunit">biostratigraphic unit</a></li>
<li><a href="#block">block</a></li>
<li><a href="#chronostratigraphicunit">chronostratigraphic unit</a></li>
<li><a href="#complex">complex</a></li>
<li><a href="#concurrentrangezone">concurrent range zone</a></li>
<li><a href="#continent">continent</a></li>
<li><a href="#craton">craton</a></li>
<li><a href="#crustalelement">crustal element</a></li>
<li><a href="#denudationalfeature">denudational feature</a></li>
<li><a href="#depression">depression</a></li>
<li><a href="#dome">dome</a></li>
<li><a href="#duplex">duplex</a></li>
<li><a href="#embayment">embayment</a></li>
<li><a href="#escarpment">escarpment</a></li>
<li><a href="#extendedcrustprovince">extended crust province</a></li>
<li><a href="#fault">fault</a></li>
<li><a href="#faultscarp">fault scarp</a></li>
<li><a href="#faultset">fault set</a></li>
<li><a href="#faultsystem">fault system</a></li>
<li><a href="#faultzone">fault zone</a></li>
<li><a href="#flow">flow</a></li>
<li><a href="#fold">fold</a></li>
<li><a href="#foldbelt">fold belt</a></li>
<li><a href="#formation">formation</a></li>
<li><a href="#geologicfeature">geologic feature</a></li>
<li><a href="#geologicalheritagesite">geological heritage site</a></li>
<li><a href="#geologicallysignificantsite">geologically significant site</a></li>
<li><a href="#geopark">geopark</a></li>
<li><a href="#geophysicaldomain">geophysical domain</a></li>
<li><a href="#geophysicalfeature">geophysical feature</a></li>
<li><a href="#georesourceaccumulation">georesource accumulation</a></li>
<li><a href="#geotrail">geotrail</a></li>
<li><a href="#graben">graben</a></li>
<li><a href="#group">group</a></li>
<li><a href="#halfgraben">half graben</a></li>
<li><a href="#horst">horst</a></li>
<li><a href="#igneousprovince">igneous province</a></li>
<li><a href="#inlier">inlier</a></li>
<li><a href="#intervalzone">interval zone</a></li>
<li><a href="#klippe">klippe</a></li>
<li><a href="#largeigneousprovince">large igneous province</a></li>
<li><a href="#lineagezone">lineage zone</a></li>
<li><a href="#lithodeme">lithodeme</a></li>
<li><a href="#lithodemicfeature">lithodemic feature</a></li>
<li><a href="#lithostratigraphicunit">lithostratigraphic unit</a></li>
<li><a href="#magnetostratigraphicpolaritysubzone">magnetostratigraphic polarity subzone</a></li>
<li><a href="#magnetostratigraphicpolaritysuperzone">magnetostratigraphic polarity superzone</a></li>
<li><a href="#magnetostratigraphicpolarityzone">magnetostratigraphic polarity zone</a></li>
<li><a href="#magnetostratigraphicunit">magnetostratigraphic unit</a></li>
<li><a href="#member">member</a></li>
<li><a href="#mineralprovince">mineral province</a></li>
<li><a href="#monocline">monocline</a></li>
<li><a href="#mylonitezone">mylonite zone</a></li>
<li><a href="#nappe">nappe</a></li>
<li><a href="#nappecomplex">nappe complex</a></li>
<li><a href="#orogen">orogen</a></li>
<li><a href="#orogeniccollage">orogenic collage</a></li>
<li><a href="#outlier">outlier</a></li>
<li><a href="#overturnedfold">overturned fold</a></li>
<li><a href="#pedostratigraphicunit">pedostratigraphic unit</a></li>
<li><a href="#peneplain">peneplain</a></li>
<li><a href="#presentcontinent">present continent</a></li>
<li><a href="#rangezone">range zone</a></li>
<li><a href="#ridge">ridge</a></li>
<li><a href="#sedimentarybasin">sedimentary basin</a></li>
<li><a href="#seismicprovince">seismic province</a></li>
<li><a href="#sequencestratigraphicunit">sequence stratigraphic unit</a></li>
<li><a href="#shearzone">shear zone</a></li>
<li><a href="#shield">shield</a></li>
<li><a href="#stratigraphicevent">stratigraphic event</a></li>
<li><a href="#stratigraphicfeature">stratigraphic feature</a></li>
<li><a href="#stratigraphicunit">stratigraphic unit</a></li>
<li><a href="#structuralfeature">structural feature</a></li>
<li><a href="#subbasin">subbasin</a></li>
<li><a href="#subgroup">subgroup</a></li>
<li><a href="#suite">suite</a></li>
<li><a href="#superbasin">superbasin</a></li>
<li><a href="#supercontinent">supercontinent</a></li>
<li><a href="#supercraton">supercraton</a></li>
<li><a href="#supergroup">supergroup</a></li>
<li><a href="#supersuite">supersuite</a></li>
<li><a href="#syncline">syncline</a></li>
<li><a href="#synclinorium">synclinorium</a></li>
<li><a href="#synform">synform</a></li>
<li><a href="#taxonrangezone">taxon range zone</a></li>
<li><a href="#tectonicentity">tectonic entity</a></li>
<li><a href="#tectonicfeature">tectonic feature</a></li>
<li><a href="#tectonicplate">tectonic plate</a></li>
<li><a href="#tectonisedmetomorphosedprovince">tectonised metomorphosed province</a></li>
<li><a href="#tectonostratigraphicentity">tectonostratigraphic entity</a></li>
<li><a href="#terrane">terrane</a></li>
<li><a href="#trough">trough</a></li>
<li><a href="#unconformity">unconformity</a></li>
<li><a href="#window">window</a></li>
</ul>
<div class="entity class" id="geologicfeature">
<h3>geologic feature<sup title="class" class="sup-c">c</sup></h3>
<table>
<tr>
<th>URI</th>
<td><code>http://sweetontology.net/realmGeol/GeologicFeature</code></td>
</tr>
<tr>
<th>Description</th>
<td>
<p>A geologic feature is a conceptual feature a that is hypothesized to exist coherently in the Earth that results from geological processes</p>
</td>
</tr>
<tr>
<th>Usage Note</th>
<td>
<p>Geologic Features include sedimentary basins, stratigraphic units, non-stratigraphic (lithodemic) units, stratigraphic event features, provinces, tectonic and structural features, georesource accumulations, and geologically significant sites, among others</p>
</td>
</tr>
<tr>
<th>Example</th>
<td>
<pre>
Individuals: Lake Eyre Basin, Sarmatian Craton, Victoria Point Sandbar, Mount Erebus Volcano. Subclasses: Basin, Craton, Shield, Province, Sub-Province
</pre>
</td>
</tr>
<tr>
<th>Sub-classes</th>
<td>
<a href="#lithodemicfeature">geof:LithodemicFeature</a><sup class="sup-c" title="class">c</sup><br/>
<a href="#geologicallysignificantsite">geof:GeologicallySignificantSite</a><sup class="sup-c" title="class">c</sup><br/>
<a href="#tectonicfeature">geof:TectonicFeature</a><sup class="sup-c" title="class">c</sup><br/>
<a href="#geophysicalfeature">geof:GeophysicalFeature</a><sup class="sup-c" title="class">c</sup><br/>
<a href="#stratigraphicfeature">geof:StratigraphicFeature</a><sup class="sup-c" title="class">c</sup><br/>
<a href="#structuralfeature">geof:StructuralFeature</a><sup class="sup-c" title="class">c</sup><br/>
<a href="#georesourceaccumulation">geof:GeoResourceAccumulation</a><sup class="sup-c" title="class">c</sup><br/>
</td>
</tr>
</table>
</div>
<div class="entity class" id="abundancezone">
<h3>abundance zone<sup title="class" class="sup-c">c</sup></h3>
<table>
<tr>
<th>URI</th>
<td><code>https://linked.data.gov.au/def/geofeatures/AbundanceZone</code></td>
</tr>
<tr>
<th>Source</th>
<td>
<a href="http://www.stratigraphy.org/index.php/ics-stratigraphicguide">http://www.stratigraphy.org/index.php/ics-stratigraphicguide</a>
</td>
</tr>
<tr>
<th>Description</th>
<td>
<p>The body of strata in which the abundance of a particular taxon or specified group of taxa is significantly greater than is usual in the adjacent parts of the section. (ICS, Online, December 2019)</p>
</td>
</tr>
<tr>
<th>Super-classes</th>
<td>
<a href="#biostratigraphicunit">geof:BiostratigraphicUnit</a><sup class="sup-c" title="class">c</sup><br/>
</td>
</tr>
</table>
</div>
<div class="entity class" id="ancientcontinent">
<h3>ancient continent<sup title="class" class="sup-c">c</sup></h3>
<table>
<tr>
<th>URI</th>
<td><code>https://linked.data.gov.au/def/geofeatures/AncientContinent</code></td>
</tr>
<tr>
<th>Source</th>
<td>
<a href="https://linked.data.gov.au/def/geofeatures">https://linked.data.gov.au/def/geofeatures</a>
</td>
</tr>
<tr>
<th>Description</th>
<td>
<p>A continent that has been recognised as being a distinct entity in the past and not as a supercontinent, and, is not recognised as a present-day continent, although it may form part of one or more (present-day continents). (Definition created here)</p>
</td>
</tr>
<tr>
<th>Super-classes</th>
<td>
<a href="#continent">geof:Continent</a><sup class="sup-c" title="class">c</sup><br/>
</td>
</tr>
</table>
</div>
<div class="entity class" id="anticline">
<h3>anticline<sup title="class" class="sup-c">c</sup></h3>
<table>
<tr>
<th>URI</th>
<td><code>https://linked.data.gov.au/def/geofeatures/Anticline</code></td>
</tr>
<tr>
<th>Source</th>
<td>
<a href="http://www.glossaryofgeology.org">http://www.glossaryofgeology.org</a>
</td>
</tr>
<tr>
<th>Description</th>
<td>
<p>A fold, generally convex upward, whose core contains the stratigraphically older rocks. (Neuendorf et al., 2011)</p>
</td>
</tr>
<tr>
<th>Super-classes</th>
<td>
<a href="#structuralfeature">geof:StructuralFeature</a><sup class="sup-c" title="class">c</sup><br/>
</td>
</tr>
</table>
</div>
<div class="entity class" id="anticlinorium">
<h3>anticlinorium<sup title="class" class="sup-c">c</sup></h3>
<table>
<tr>
<th>URI</th>
<td><code>https://linked.data.gov.au/def/geofeatures/Anticlinorium</code></td>
</tr>
<tr>
<th>Source</th>
<td>
<a href="http://www.glossaryofgeology.org">http://www.glossaryofgeology.org</a>
</td>
</tr>
<tr>
<th>Description</th>
<td>
<p>A composite anticlinal structure of regional extent composed of lesser folds. (Neuendorf et al., 2011)</p>
</td>
</tr>
<tr>
<th>Super-classes</th>
<td>
<a href="#structuralfeature">geof:StructuralFeature</a><sup class="sup-c" title="class">c</sup><br/>
</td>
</tr>
</table>
</div>
<div class="entity class" id="antiform">
<h3>antiform<sup title="class" class="sup-c">c</sup></h3>
<table>
<tr>
<th>URI</th>
<td><code>https://linked.data.gov.au/def/geofeatures/Antiform</code></td>
</tr>
<tr>
<th>Source</th>
<td>
<a href="http://www.glossaryofgeology.org">http://www.glossaryofgeology.org</a>
</td>
</tr>
<tr>
<th>Description</th>
<td>
<p>Any convex-upward, concave downward fold. The term is usually used when the folded layers do not possess a stratigraphic order, when the stratigraphic order of the folded layers is not known, or when the fold core also contains the stratigraphically younger rock. (Neuendorf et al., 2011)</p>
</td>
</tr>
<tr>
<th>Super-classes</th>
<td>
<a href="#structuralfeature">geof:StructuralFeature</a><sup class="sup-c" title="class">c</sup><br/>
</td>
</tr>
</table>
</div>
<div class="entity class" id="antiformalstack">
<h3>antiformal stack<sup title="class" class="sup-c">c</sup></h3>
<table>
<tr>
<th>URI</th>
<td><code>https://linked.data.gov.au/def/geofeatures/AntiformalStack</code></td>
</tr>
<tr>
<th>Source</th>
<td>
<a href="http://www.glossaryofgeology.org">http://www.glossaryofgeology.org</a>
</td>
</tr>
<tr>
<th>Description</th>
<td>
<p>A duplex in which the trailing branch lines coincide and the leading branch lines either nearly coincide or lie vertically above each other. This results in a stack of horses and leads to a local culmination in thrust sheet. (Neuendorf et al. (2011) citing Boyer & Elliott (1982))</p>
</td>
</tr>
<tr>
<th>Super-classes</th>
<td>
<a href="#structuralfeature">geof:StructuralFeature</a><sup class="sup-c" title="class">c</sup><br/>
</td>
</tr>
</table>
</div>
<div class="entity class" id="arch">
<h3>arch<sup title="class" class="sup-c">c</sup></h3>
<table>
<tr>
<th>URI</th>
<td><code>https://linked.data.gov.au/def/geofeatures/Arch</code></td>
</tr>
<tr>
<th>Source</th>
<td>
<a href="http://www.glossaryofgeology.org">http://www.glossaryofgeology.org</a>
</td>
</tr>
<tr>
<th>Description</th>
<td>
<p>A broad, open anticlinal fold on a regional scale; it is usually a basement doming. (Neuendorf et al., 2011)</p>
</td>
</tr>
<tr>
<th>Super-classes</th>
<td>
<a href="#structuralfeature">geof:StructuralFeature</a><sup class="sup-c" title="class">c</sup><br/>
</td>
</tr>
</table>
</div>
<div class="entity class" id="assemblagezone">
<h3>assemblage zone<sup title="class" class="sup-c">c</sup></h3>
<table>
<tr>
<th>URI</th>
<td><code>https://linked.data.gov.au/def/geofeatures/AssemblageZone</code></td>
</tr>
<tr>
<th>Source</th>
<td>
<a href="http://www.stratigraphy.org/index.php/ics-stratigraphicguide">http://www.stratigraphy.org/index.php/ics-stratigraphicguide</a>
</td>
</tr>
<tr>
<th>Description</th>
<td>
<p>The body of strata characterized by an assemblage of three or more fossil taxa that, taken together, distinguishes it in biostratigraphic character from adjacent strata. (ICS, Online, December 2019)</p>
</td>
</tr>
<tr>
<th>Super-classes</th>
<td>
<a href="#biostratigraphicunit">geof:BiostratigraphicUnit</a><sup class="sup-c" title="class">c</sup><br/>
</td>
</tr>
</table>
</div>
<div class="entity class" id="associationzone">
<h3>association zone<sup title="class" class="sup-c">c</sup></h3>
<table>
<tr>
<th>URI</th>
<td><code>https://linked.data.gov.au/def/geofeatures/AssociationZone</code></td>
</tr>
<tr>
<th>Source</th>
<td>
<a href="https://doi.org/10.1080/01916122.2012.718609">https://doi.org/10.1080/01916122.2012.718609</a>
</td>
</tr>
<tr>
<th>Description</th>
<td>
<p>The body of strata between two designated biostratigraphical horizons, which represent the boundaries of the unit and separate it from any preceding or succeeding biozone. These bounding horizons may be delimited individually by: the level of the first stratigraphical appearance (lowermost or oldest occurrence) of a specified taxon (species, genus) in any one stratigraphical section; or another specified biostratigraphical feature considered to approximate a time horizon. The zone is further delimited by specified taxa (preferably, at least three), which have first appearances within the zone. (de Jersey & McKellar, 2013; Bomfleur et al., 2014)</p>
</td>
</tr>
<tr>
<th>Super-classes</th>
<td>
<a href="#biostratigraphicunit">geof:BiostratigraphicUnit</a><sup class="sup-c" title="class">c</sup><br/>
</td>
</tr>
</table>
</div>
<div class="entity class" id="bed">
<h3>bed<sup title="class" class="sup-c">c</sup></h3>
<table>
<tr>
<th>URI</th>
<td><code>https://linked.data.gov.au/def/geofeatures/Bed</code></td>
</tr>
<tr>
<th>Source</th>
<td>
<a href="https://doi.org/10.1130/9780813774022">https://doi.org/10.1130/9780813774022</a>
</td>
</tr>
<tr>
<th>Description</th>
<td>
<p>Bed (Beds) is the smallest formal unit in the hierarchy of sedimentary lithostratigraphic units, e.g. a single stratum lithologically distinguishable from other layers above and below (Salvador, 2013; ICS Online, January 2020). Customarily, only distinctive beds (commonly known as marker beds), which are particularly useful for stratigraphic purposes, like correlation or reference, are given proper names and considered formal lithostratigraphic units (Staines, 1985)</p>
</td>
</tr>
<tr>
<th>Super-classes</th>
<td>
<a href="#lithostratigraphicunit">geof:LithostratigraphicUnit</a><sup class="sup-c" title="class">c</sup><br/>
</td>
</tr>
</table>
</div>
<div class="entity class" id="beds">
<h3>beds<sup title="class" class="sup-c">c</sup></h3>
<table>
<tr>
<th>URI</th>
<td><code>https://linked.data.gov.au/def/geofeatures/Beds</code></td>
</tr>
<tr>
<th>Source</th>
<td>
<a href="https://doi.org/10.1080/08120098508729316">https://doi.org/10.1080/08120098508729316</a>
</td>
</tr>
<tr>
<th>Description</th>
<td>
<p>beds (uncapitalised): an informal unit applied to a sequence of poorly known strata until further work is carried out, as advised in the Field Geologist’s Guide to Lithostratigraphic Nomenclature in Australia (Staines, 1985), and endorsed by the Stratigraphic Nomenclature Committee, Geological Society of Australia.</p>
</td>
</tr>
<tr>
<th>Super-classes</th>
<td>
<a href="#lithostratigraphicunit">geof:LithostratigraphicUnit</a><sup class="sup-c" title="class">c</sup><br/>
</td>
</tr>
</table>
</div>
<div class="entity class" id="biostratigraphicunit">
<h3>biostratigraphic unit<sup title="class" class="sup-c">c</sup></h3>
<table>
<tr>
<th>URI</th>
<td><code>https://linked.data.gov.au/def/geofeatures/BiostratigraphicUnit</code></td>
</tr>
<tr>
<th>Source</th>
<td>
<a href="http://www.stratigraphy.org/index.php/ics-stratigraphicguide">http://www.stratigraphy.org/index.php/ics-stratigraphicguide</a>
</td>
</tr>
<tr>
<th>Description</th>
<td>
<p>Biostratigraphic units/Biostratigraphic Zones (biozones) are bodies of strata that are defined or characterized on the basis of their contained fossils. The different types have no hierarchical significance, and are not based on mutually exclusive criteria. (ICS, Online, December 2019)</p>
</td>
</tr>
<tr>
<th>Super-classes</th>
<td>
<a href="#stratigraphicunit">geof:StratigraphicUnit</a><sup class="sup-c" title="class">c</sup><br/>
</td>
</tr>
<tr>
<th>Sub-classes</th>
<td>
<a href="#assemblagezone">geof:AssemblageZone</a><sup class="sup-c" title="class">c</sup><br/>
<a href="#lineagezone">geof:LineageZone</a><sup class="sup-c" title="class">c</sup><br/>
<a href="#concurrentrangezone">geof:ConcurrentRangeZone</a><sup class="sup-c" title="class">c</sup><br/>
<a href="#associationzone">geof:AssociationZone</a><sup class="sup-c" title="class">c</sup><br/>
<a href="#intervalzone">geof:IntervalZone</a><sup class="sup-c" title="class">c</sup><br/>
<a href="#taxonrangezone">geof:TaxonRangeZone</a><sup class="sup-c" title="class">c</sup><br/>
<a href="#rangezone">geof:RangeZone</a><sup class="sup-c" title="class">c</sup><br/>
<a href="#abundancezone">geof:AbundanceZone</a><sup class="sup-c" title="class">c</sup><br/>
</td>
</tr>
</table>
</div>
<div class="entity class" id="block">
<h3>block<sup title="class" class="sup-c">c</sup></h3>
<table>
<tr>
<th>URI</th>
<td><code>https://linked.data.gov.au/def/geofeatures/Block</code></td>
</tr>
<tr>
<th>Source</th>
<td>
<a href="http://www.glossaryofgeology.org">http://www.glossaryofgeology.org</a>
</td>
</tr>
<tr>
<th>Description</th>
<td>
<p>A block of the crust that has been displaced by movement on a fault. (Neuendorf et al., 2011)</p>
</td>
</tr>
<tr>
<th>Super-classes</th>
<td>
<a href="#structuralfeature">geof:StructuralFeature</a><sup class="sup-c" title="class">c</sup><br/>
</td>
</tr>
</table>
</div>
<div class="entity class" id="chronostratigraphicunit">
<h3>chronostratigraphic unit<sup title="class" class="sup-c">c</sup></h3>
<table>
<tr>
<th>URI</th>
<td><code>https://linked.data.gov.au/def/geofeatures/ChronostratigraphicUnit</code></td>
</tr>
<tr>
<th>Source</th>
<td>
<a href="http://www.stratigraphy.org/index.php/ics-stratigraphicguide">http://www.stratigraphy.org/index.php/ics-stratigraphicguide</a>
</td>
</tr>
<tr>
<th>Description</th>
<td>
<p>As the term implies, Chronostratigraphic Units are Time-Rock Units. They are bodies of rocks, layered or unlayered, that were formed during a specified interval of geologic time. [The units of geologic time during which chronostratigraphic units were formed are called geochronologic (geological-time) units.] (ICS, Online, December, 2019). NB: The North American Stratigraphic Code (2005) and Owen (2009) advise that geochronologic units should only be associated with Lithodemic (non-stratigraphic) Units.</p>
</td>
</tr>
<tr>
<th>Super-classes</th>
<td>
<a href="#stratigraphicunit">geof:StratigraphicUnit</a><sup class="sup-c" title="class">c</sup><br/>
</td>
</tr>
</table>
</div>
<div class="entity class" id="complex">
<h3>complex<sup title="class" class="sup-c">c</sup></h3>
<table>
<tr>
<th>URI</th>
<td><code>https://linked.data.gov.au/def/geofeatures/Complex</code></td>
</tr>
<tr>
<th>Source</th>
<td>
<a href="https://doi.org/10.1080/11035897.2016.1178666">https://doi.org/10.1080/11035897.2016.1178666</a>
</td>
</tr>
<tr>
<th>Description</th>
<td>
<p>In the classification of Kumpulainen (2016), a complex is a non-ranked lithodemic unit that corresponds to a suite or supersuite. Its usage applies to the organisation and classification of an assemblage of two or more genetically different rock types (i.e. igneous, metamorphic and/or sedimentary). For example, a tectonic amalgamation of igneous, sedimentary and metamorphic rocks may form a structural complex; and a volcanic complex may comprise extrusive, sedimentary and the related intrusive components.</p>
</td>
</tr>
<tr>
<th>Super-classes</th>
<td>
<a href="#lithodemicfeature">geof:LithodemicFeature</a><sup class="sup-c" title="class">c</sup><br/>
</td>
</tr>
</table>
</div>
<div class="entity class" id="concurrentrangezone">
<h3>concurrent range zone<sup title="class" class="sup-c">c</sup></h3>
<table>
<tr>
<th>URI</th>
<td><code>https://linked.data.gov.au/def/geofeatures/ConcurrentRangeZone</code></td>
</tr>
<tr>
<th>Source</th>
<td>
<a href="http://www.stratigraphy.org/index.php/ics-stratigraphicguide">http://www.stratigraphy.org/index.php/ics-stratigraphicguide</a>
</td>
</tr>
<tr>
<th>Description</th>
<td>
<p>The body of strata including the overlapping parts of the range zones of two specified taxa. (ICS, Online, December 2019)</p>
</td>
</tr>
<tr>
<th>Super-classes</th>
<td>
<a href="#biostratigraphicunit">geof:BiostratigraphicUnit</a><sup class="sup-c" title="class">c</sup><br/>
</td>
</tr>
</table>
</div>
<div class="entity class" id="continent">
<h3>continent<sup title="class" class="sup-c">c</sup></h3>
<table>
<tr>
<th>URI</th>
<td><code>https://linked.data.gov.au/def/geofeatures/Continent</code></td>
</tr>
<tr>
<th>Source</th>
<td>
<a href="http://www.glossaryofgeology.org">http://www.glossaryofgeology.org</a>
</td>
</tr>
<tr>
<th>Description</th>
<td>
<p>One of Earth’s major landmasses (or former major landmasses), including continental shelves. (Neuendorf et al., 2011; Blewett, 2012). The Australian Continent, as an example, is divided into fundamental geological elements embracing geological provinces.</p>
</td>
</tr>
<tr>
<th>Super-classes</th>
<td>
<a href="#tectonicentity">geof:TectonicEntity</a><sup class="sup-c" title="class">c</sup><br/>
</td>
</tr>
<tr>
<th>Sub-classes</th>
<td>
<a href="#ancientcontinent">geof:AncientContinent</a><sup class="sup-c" title="class">c</sup><br/>
<a href="#presentcontinent">geof:PresentContinent</a><sup class="sup-c" title="class">c</sup><br/>
</td>
</tr>
</table>
</div>
<div class="entity class" id="craton">
<h3>craton<sup title="class" class="sup-c">c</sup></h3>
<table>
<tr>
<th>URI</th>
<td><code>https://linked.data.gov.au/def/geofeatures/Craton</code></td>
</tr>
<tr>
<th>Source</th>
<td>
<a href="http://www.glossaryofgeology.org">http://www.glossaryofgeology.org</a>
</td>
</tr>
<tr>
<th>Description</th>
<td>
<p>A craton is part of Earth's continental crust that has attained stability and has been little deformed for a prolonged period. Cratons include shield areas, where Precambrian rocks are exposed, and platform areas, where Precambrian rocks are overlain by a thin layer of Phanerozoic strata. (Neuendorf et al., 2011)</p>
</td>
</tr>
<tr>
<th>Super-classes</th>
<td>
<a href="#tectonicentity">geof:TectonicEntity</a><sup class="sup-c" title="class">c</sup><br/>
</td>
</tr>
</table>
</div>
<div class="entity class" id="crustalelement">
<h3>crustal element<sup title="class" class="sup-c">c</sup></h3>
<table>
<tr>
<th>URI</th>
<td><code>https://linked.data.gov.au/def/geofeatures/CrustalElement</code></td>
</tr>
<tr>
<th>Source</th>
<td>
<a href="http://pid.geoscience.gov.au/dataset/ga/14909">http://pid.geoscience.gov.au/dataset/ga/14909</a>
</td>