Baikal orogeny

E473725

Baikal orogeny is an ancient mountain-building event that shaped parts of Siberia and Central Asia during the late Precambrian to early Paleozoic eras.

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All labels observed (1)

Label Occurrences
Baikal orogeny canonical 1

Statements (39)

Predicate Object
instanceOf geological event
mountain-building event
orogeny
affects Central Asian orogenic belt NERFINISHED
Siberian craton margins NERFINISHED
associatedWith Baikal mountain belt NERFINISHED
Baikalides NERFINISHED
chronologicalPosition late Precambrian–early Paleozoic
endTime early Paleozoic
geologicalAgeContext Cambrian
Neoproterozoic NERFINISHED
hasEffect crustal thickening
folding and thrusting of crustal rocks
formation of mountain belts
granitoid magmatism
metamorphism of sedimentary sequences
hasResult reworking of Precambrian basement complexes
stabilization of parts of the Siberian continental crust
hasStratigraphicSignificance controls distribution of Neoproterozoic–Cambrian basins
defines regional unconformities in Siberia
involvesProcess continental collision
subduction
terrane accretion
namedAfter Lake Baikal region NERFINISHED
occursIn Central Asia NERFINISHED
Siberia NERFINISHED
partOf tectonic evolution of Central Asia
tectonic evolution of Siberia
precedes Caledonian orogeny NERFINISHED
produced granite intrusions in Siberia
metamorphic belts in Baikal region
relatedTo Cadomian orogeny NERFINISHED
Pan-African orogeny NERFINISHED
startTime late Precambrian
studiedInDiscipline historical geology
structural geology
tectonics
tectonicSetting accretionary orogeny
continental margin orogeny

Referenced by (1)

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

Baikal Mountains orogeny Baikal orogeny