Main Boundary Thrust zone

E206913

The Main Boundary Thrust zone is a major geological fault system in the Himalayas that marks a key tectonic boundary where the Indian Plate is thrust beneath the Eurasian Plate.

All labels observed (1)

Label Occurrences
Main Boundary Thrust zone canonical 1

How this entity was disambiguated

Statements (41)

Predicate Object
instanceOf geological fault system
tectonic boundary
thrust fault
alsoKnownAs MBT
Main Boundary Thrust
associatedWith Himalayan seismicity
fold‑and‑thrust belt deformation
continent Asia
controls topographic break between Lesser Himalaya and Siwalik Hills
deformationStyle thin‑skinned tectonics
displaces Siwalik Group sediments
extendsThrough Bhutan
India
Nepal
Pakistan
eastern Himalaya region
faultType north‑dipping thrust fault
formedBy collision of Indian Plate and Eurasian Plate
geologicalAge Cenozoic
lithosphericPlatesInvolved Eurasian Plate
India Plate
surface form: Indian Plate
locatedIn Himalayas
marksBoundaryBetween Eurasian Plate
India Plate
surface form: Indian Plate
movementType compressional
olderThan Himalayan Frontal Thrust
orientation generally east‑west
overthrusts Lesser Himalayan rocks onto Siwalik rocks
partOf Himalayan orogeny
surface form: Himalayan orogen
region South Asia
relatedStructure Himalayan Frontal Thrust
Main Central Thrust
separates Lesser Himalayas
surface form: Lesser Himalaya

Sub‑Himalaya
significance major structural boundary within Himalayan orogenic wedge
studiedInDiscipline seismology
structural geology
tectonics
tectonicRole accommodates crustal shortening between India and Eurasia
tectonicSetting convergent plate boundary
youngerThan Main Central Thrust

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 Boundary Thrust zone