Marathon orogeny

E402691

The Marathon orogeny was a late Paleozoic mountain-building event in what is now western Texas, associated with the collision of continental plates during the assembly of the supercontinent Pangaea.

All labels observed (2)

Label Occurrences
Marathon orogen 1
Marathon orogeny canonical 1

How this entity was disambiguated

Statements (32)

Predicate Object
instanceOf geological event
mountain-building event
orogeny
age approximately 320–270 million years ago
associatedWith assembly of the supercontinent Pangaea
cause collision of continental plates
continent Gondwana
Laurentia
deforms Paleozoic sedimentary rocks
geologicalPeriod Late Paleozoic
Pennsylvanian
Permian Period
surface form: Permian
locatedIn United States of America
surface form: United States

western Texas
orogenicBelt Marathon fold-and-thrust belt
overprints earlier passive-margin strata
partOf Ouachita orogeny
surface form: Ouachita orogenic belt

late Paleozoic orogenies of North America
preservedIn Marathon Basin
Trans-Pecos region
surface form: Trans-Pecos Texas
relatedTo Appalachian orogeny
surface form: Alleghanian orogeny

Ouachita orogeny
Variscan orogeny
researchField regional geology of Texas
structural geology
tectonics
resultedIn crustal shortening
fold-and-thrust deformation of Paleozoic strata
uplift of the Marathon region
significance records late stages of Pangaea assembly in southern Laurentia
structuralStyle thin-skinned tectonics
tectonicSetting convergent plate margin

How these facts were elicited

Referenced by (2)

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

Ouachita orogeny relatedTo Marathon orogeny
Appalachian–Ouachita–Marathon orogenic system hasPart Marathon orogeny
this entity surface form: Marathon orogen