Panthalassa Ocean margins

E727680

The Panthalassa Ocean margins were the extensive continental and volcanic arc boundaries of the vast Panthalassa superocean that surrounded the supercontinent Pangaea during much of the Mesozoic Era.

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Statements (47)

Predicate Object
instanceOf ancient ocean margin system
paleogeographic feature
associatedWith Mesozoic accretionary orogens
accretionary prisms
back-arc basins
convergent plate boundaries
forearc basins
subduction zones
associatedWithProcess arc magmatism
continental growth by accretion
oceanic lithosphere subduction
sedimentary basin formation
characterizedBy arc–continent collisions
extensive magmatism
long-lived subduction
orogenic belts
evolvedInto proto-Pacific margins
existedDuring Late Paleozoic NERFINISHED
Mesozoic Era NERFINISHED
hadBoundaryType continental margin
volcanic arc margin
influenced Mesozoic plate reorganization
distribution of Mesozoic magmatic arcs
growth of continental crust around the Pacific
linkedTo assembly of Pangaea
breakup of Pangaea
paleogeographicPosition global, encircling Pangaea
partOf Panthalassa Ocean NERFINISHED
preceded modern circum-Pacific margins
recordPreservedIn accreted terranes
circum-Pacific orogens
orogenic belts of East Asia
orogenic belts of New Zealand
orogenic belts of eastern Australia
orogenic belts of western North America
relatedTo Pacific Ocean margins NERFINISHED
Pangaea margins
relatedToConcept supercontinent cycle
superocean
scale planetary-scale margin system
studiedIn orogenic geology
paleogeography
paleotectonics
surrounded Pangaea NERFINISHED
tectonicSetting circum-Pangaean
timeSpan Late Paleozoic to Early Mesozoic
primarily Triassic to Jurassic

Referenced by (1)

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

Toarcian Oceanic Anoxic Event hasGlobalExtent Panthalassa Ocean margins