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 ⓘ
linked to: Permian Period
locatedIn United States ⓘ
western Texas ⓘ
orogenicBelt Marathon fold-and-thrust belt ⓘ
overprints earlier passive-margin strata ⓘ
partOf Ouachita orogenic belt ⓘ
linked to: Ouachita orogeny

late Paleozoic orogenies of North America ⓘ
preservedIn Marathon Basin ⓘ
Trans-Pecos Texas ⓘ
linked to: Trans-Pecos region
relatedTo Alleghanian orogeny ⓘ
linked to: Appalachian 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 orogen ⓘ
linked to: Marathon orogeny