Main Central Thrust zone

E206912

The Main Central Thrust zone is a major tectonic fault system in the Himalayas that marks a key boundary where high-grade metamorphic rocks have been thrust over lower-grade rocks during the Himalayan mountain-building process.

All labels observed (1)

Label Occurrences
Main Central Thrust zone canonical 1

How this entity was disambiguated

Statements (37)

Predicate Object
instanceOf geological structure
tectonic fault zone
thrust fault
associatedWith Himalayan mountain‑building
continental collision of India and Eurasia
extendsAlongStrike over 1500 km
formedDuring Cenozoic
surface form: Cenozoic Era
hasDeformationStyle brittle‑ductile faulting
ductile shearing
hasKinematics top‑to‑the‑south shear sense
hasMetamorphicGrade high‑grade
medium‑grade
hasRockType gneiss
migmatite
schist
hasSignificance key marker of Himalayan tectonic evolution
major crustal‑scale shear zone
isKeyFor reconstructing India–Eurasia collision history
understanding exhumation of Greater Himalayan rocks
locatedIn Bhutan
Himalayas
India
Nepal
marksBoundaryBetween Greater Himalayas
surface form: Greater Himalayan Sequence

Lesser Himalayas
surface form: Lesser Himalayan Sequence
movementType north‑directed thrusting
south‑vergent shortening
overthrusts Lesser Himalayan rocks
partOf Alpine-Himalayan orogenic belt
surface form: Himalayan orogen
relatedTo Main Boundary Thrust
South Tibetan Detachment System
separates high‑grade metamorphic rocks
lower‑grade metamorphic rocks
studiedInDiscipline metamorphic petrology
structural geology
tectonics
tectonicSetting convergent plate boundary

How these facts were elicited

Referenced by (1)

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

Himalayan orogeny produces Main Central Thrust zone