Taimyr Orogen

E781776

The Taimyr Orogen is a major Paleozoic mountain belt in the Taimyr Peninsula of Arctic Siberia, formed by tectonic collisions along the northern margin of the Siberian Craton.

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Statements (39)

Predicate Object
instanceOf geologic province
mountain belt
orogen
associatedWith Siberian Craton NERFINISHED
boundedBy Siberian Craton to the south
contains deformed sedimentary rocks
igneous intrusions
metamorphic rocks
evidenceFrom field mapping
geochronology
petrology
structural analysis
extendsAcross central Taimyr Peninsula NERFINISHED
formedBy plate convergence
tectonic collisions
geologicPeriod Paleozoic NERFINISHED
hasImportanceFor reconstructing Paleozoic paleogeography of Siberia
understanding the assembly of Arctic continental blocks
hasTectonicStyle crustal shortening
folding
thrusting
isInContinent Asia NERFINISHED
isInCountry Russia NERFINISHED
isInRegion Russian Arctic NERFINISHED
locatedIn Arctic Siberia NERFINISHED
Taimyr Peninsula NERFINISHED
locatedOn northern margin of the Siberian Craton
marginType northern passive-to-active margin of the Siberian Craton
minimumAge Paleozoic
orogenyAge Paleozoic
overprints older basement of the Siberian Craton margin
partOf Siberian Arctic orogenic systems NERFINISHED
relatedTo Arctic orogenic belts NERFINISHED
Paleozoic plate reconstructions of the Arctic
researchField regional geology
structural geology
tectonics
significance records Paleozoic tectonic evolution of the northern Siberian margin
tectonicSetting collisional orogen

Referenced by (1)

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

Siberian Craton boundedBy Taimyr Orogen