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 8
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 (11)

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
Iberian Massif → orogenyRecorded → Cadomian orogeny ⓘ
Baikal orogeny → relatedTo → Cadomian orogeny ⓘ
Brunovistulian terrane → relatedTo → Cadomian orogeny ⓘ