Irish Caledonides

E842648

The Irish Caledonides are a mountain belt in Ireland formed during the Caledonian orogeny, representing deformed and metamorphosed remnants of ancient oceanic and continental crust.

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Statements (43)

Predicate Object
instanceOf mountain belt
ageRange Ordovician
Silurian
contains ancient continental crust remnants
ancient oceanic crust remnants
deformed crust
metamorphosed crust
exposedIn northwest Ireland
western Ireland NERFINISHED
extendsInto Greenland NERFINISHED
Scandinavia NERFINISHED
Scotland NERFINISHED
formedBy continental collision
crustal thickening
subduction
formedDuring Caledonian orogeny NERFINISHED
geologicalAge Paleozoic
hasEconomicInterest mineral exploration
hasEvidenceFor closure of the Iapetus Ocean
hasMetamorphicGrade high-grade metamorphism
low-grade metamorphism
medium-grade metamorphism
hasProcess faulting
folding
regional metamorphism
hasRockType igneous rocks
metamorphic rocks
sedimentary rocks
hasStructure fold belts
thrust belts
isRemnantOf ancient mountain chain
locatedIn Ireland NERFINISHED
orogenyType collisional orogeny
overlainBy younger sedimentary basins in Ireland
partOf Caledonides NERFINISHED
North Atlantic Caledonides NERFINISHED
relatedTo Appalachian–Caledonian orogen NERFINISHED
Iapetus Ocean NERFINISHED
significantFor Paleozoic tectonic evolution of Ireland
studiedInDiscipline metamorphic petrology
structural geology
tectonics
tectonicSetting convergent plate margin

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Iapetus Ocean marginPreservedIn Irish Caledonides