Main Central Thrust

E753966

The Main Central Thrust is a major Himalayan tectonic fault that marks the boundary between high-grade metamorphic rocks of the Higher Himalaya and lower-grade rocks of the Lesser Himalaya.

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Statements (40)

Predicate Object
instanceOf Himalayan tectonic feature
geological structure
tectonic fault
thrust fault
age Cenozoic
associatedWith ductile deformation
metamorphic grade increase towards the hanging wall
regional metamorphism
shear zone development
displacementSense southward transport of Higher Himalayan rocks over Lesser Himalayan rocks
extendsThrough Bhutan NERFINISHED
India NERFINISHED
Nepal NERFINISHED
Pakistan‑administered Himalayan region
faultType north‑dipping thrust
formedDuring Himalayan orogeny
hasSignificance key marker for Himalayan tectonic evolution
major crustal‑scale discontinuity in the Himalaya
lithologyAbove high‑grade gneisses and schists
lithologyBelow low‑ to medium‑grade metasedimentary rocks
locatedIn Himalayas
marksBoundaryBetween high‑grade metamorphic rocks of the Higher Himalaya
lower‑grade rocks of the Lesser Himalaya
movementType compressional
namedAfter its position as a major central thrust within the Himalayan belt
overlies Lesser Himalayan Sequence NERFINISHED
parallelTo Main Boundary Thrust NERFINISHED
South Tibetan Detachment System NERFINISHED
partOf Himalayan orogenic belt NERFINISHED
region Central Himalaya NERFINISHED
relatedConcept orogenic wedge
thrust belt
relatedTo India–Eurasia plate collision NERFINISHED
separates Higher Himalaya NERFINISHED
Lesser Himalaya NERFINISHED
studiedInDiscipline metamorphic petrology
structural geology
tectonics
tectonicSetting continent‑continent collision zone
underlies Higher Himalayan Crystalline Sequence NERFINISHED

Referenced by (2)

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

Main Boundary Thrust zone youngerThan Main Central Thrust
Main Boundary Thrust zone relatedStructure Main Central Thrust