@prefix qx8: <http://data.loterre.fr/ark:/67375/QX8> .
@prefix skos: <http://www.w3.org/2004/02/skos/core#> .

qx8: a skos:ConceptScheme .
qx8:-8567VJBG-8
  skos:prefLabel "tectonic structure"@en, "structure tectonique"@fr ;
  a skos:Concept ;
  skos:narrower qx8:-TWFK7VS6-F .

qx8:-TWFK7VS6-F
  skos:exactMatch <http://data.loterre.fr/ark:/67375/26L-WJ0F8TTP-G>, <https://en.wikipedia.org/wiki/Anticline>, <https://fr.wikipedia.org/wiki/Anticlinal> ;
  skos:definition "In structural geology, an anticline is a type of fold that is an arch-like shape and has its oldest beds at its core, whereas a syncline is the inverse of an anticline. A typical anticline is convex up in which the hinge or crest is the location where the curvature is greatest, and the limbs are the sides of the fold that dip away from the hinge. Anticlines can be recognized and differentiated from antiforms by a sequence of rock layers that become progressively older toward the center of the fold. Therefore, if age relationships between various rock strata are unknown, the term antiform should be used. (Adapted from: <a href=\"https://en.wikipedia.org/wiki/Anticline\">https://en.wikipedia.org/wiki/Anticline</a>)"@en, "Un anticlinal est une structure géologique consistant en un pli convexe dont le cœur est occupé par les couches géologiques les plus anciennes. Cela signifie que le terme « anticlinal » prend en considération une notion stratigraphique, donc chronologique et pas géométrique. Un anticlinal peut donc dans de rares cas avoir une charnière de pli vers le bas (synforme). (Adapté de : <a href=\"https://fr.wikipedia.org/wiki/Anticlinal\">https://fr.wikipedia.org/wiki/Anticlinal</a>)"@fr ;
  skos:prefLabel "anticline"@en, "anticlinal"@fr ;
  a skos:Concept ;
  skos:broader qx8:-8567VJBG-8 ;
  skos:inScheme qx8: .