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.

All labels observed (1)

Label Occurrences
Irish Caledonides canonical 1

How this entity was disambiguated

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 ⓘ
linked to: Western Ireland
extendsInto Greenland ⓘ
Scandinavia ⓘ
Scotland ⓘ
formedBy continental collision ⓘ
crustal thickening ⓘ
subduction ⓘ
formedDuring Caledonian orogeny ⓘ
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 ⓘ
orogenyType collisional orogeny ⓘ
overlainBy younger sedimentary basins in Ireland ⓘ
partOf Caledonides ⓘ
North Atlantic Caledonides ⓘ
relatedTo Appalachian–Caledonian orogen ⓘ
linked to: Appalachian orogeny

Iapetus Ocean ⓘ
significantFor Paleozoic tectonic evolution of Ireland ⓘ
studiedInDiscipline metamorphic petrology ⓘ
structural geology ⓘ
tectonics ⓘ
tectonicSetting convergent plate margin ⓘ

How these facts were elicited

Referenced by (1)

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

Iapetus Ocean → marginPreservedIn → Irish Caledonides ⓘ