Cadomian orogeny

E231238

The Cadomian orogeny was a late Neoproterozoic mountain-building event that shaped parts of what are now western Europe, contributing to the assembly of the supercontinent Pannotia.

All labels observed (3)

Label Occurrences
Cadomian orogeny canonical 5
Cadomian basement 2
Cadomian belt 1

How this entity was disambiguated

Statements (45)

Predicate Object
instanceOf Neoproterozoic orogeny
geological event
orogeny
affectedLithology Neoproterozoic volcanic and sedimentary sequences
gneisses
granites
schists
affectedRegion Armorican Massif
Bohemian Massif
Channel Islands
Iberian Massif
Normandy
northern France
southern England
approximateAge circa 650–540 million years ago
associatedWith Cadomian basement
linked to: Cadomian orogeny

Neoproterozoic arc terranes of western Europe
formation of peri-Gondwanan terranes
causedBy subduction of oceanic crust beneath a continental margin
chronologicalPosition older than the Caledonian orogeny
pre-dates the Variscan orogeny
contributedTo assembly of the supercontinent Pannotia
endTime late Neoproterozoic
followedBy Pan-African orogeny
geologicalPeriod Neoproterozoic
linked to: Neoproterozoic Era
linkedTo Pan-African orogeny
locatedIn western Europe
linked to: Western Europe
namedAfter Cadomian belt
linked to: Cadomian orogeny
partOf Pan-African orogenic cycle
linked to: Pan-African orogeny

assembly of Pannotia
precededBy Grenvillian orogeny
linked to: Grenville orogeny
relatedTo Avalonian–Cadomian orogenic belt
resultedIn accretion of terranes to the West African Craton margin
crustal thickening
granitoid intrusions
magmatism
metamorphism
volcanic arc complexes
significance contributed to the early basement framework of western Europe
records late Neoproterozoic plate convergence along the northern margin of Gondwana
startTime late Neoproterozoic
structuralStyle fold-and-thrust belt deformation
high-grade metamorphic core zones
tectonicSetting active continental margin
subduction-related arc

How these facts were elicited

Referenced by (8)

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

Pannotia associatedWithOrogeny Cadomian orogeny
subject linked to: supercontinent Pannotia
Pan-African orogeny linkedTo Cadomian orogeny
Pannotia associatedOrogeny Cadomian orogeny
Cadomian orogeny namedAfter Cadomian belt
linked to: Cadomian orogeny
Cadomian orogeny associatedWith Cadomian basement
linked to: Cadomian orogeny
Moravo–Silesian Zone orogeny Cadomian orogeny
Armorican Massif orogeny Cadomian orogeny
Armorican Massif contains Cadomian basement
linked to: Cadomian orogeny