Sagaing Fault

E770666

The Sagaing Fault is a major continental transform fault in Myanmar that accommodates much of the tectonic motion between the Burma Plate and the Sunda Plate, making it a significant source of regional seismic activity.

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Statements (43)

Predicate Object
instanceOf continental fault
strike-slip fault
transform fault
accommodatesMotionBetween Burma Plate NERFINISHED
Sunda Plate NERFINISHED
affects infrastructure in central Myanmar
population centres along its trace
approximateLength ~1200 km
associatedWith shallow crustal earthquakes
country Myanmar
displacementRate on the order of tens of millimetres per year
extendsFrom northern Myanmar
extendsTo southern Myanmar NERFINISHED
faultZoneWidth several kilometres
geologicalAge Cenozoic activity
hasEarthquakePotential large damaging earthquakes
hasSegment central Sagaing Fault segment
northern Sagaing Fault segment
southern Sagaing Fault segment
isMajorSourceOf regional seismic activity in Myanmar
isMonitoredBy seismological networks in Myanmar
isStudiedIn tectonics of Southeast Asia
knownFor high seismic risk to major Myanmar cities
locatedIn Burma Plate NERFINISHED
Sunda Plate boundary region NERFINISHED
motionType right-lateral strike-slip
movementStyle horizontal displacement dominated
orientation roughly north-south
parallelTo Irrawaddy River NERFINISHED
partOf plate boundary system between India, Burma, and Sunda plates
plateBoundaryType transform
region Southeast Asia
riskType earthquake hazard
runsNear Bago NERFINISHED
Mandalay NERFINISHED
Sagaing NERFINISHED
Yangon NERFINISHED
runsThrough central Myanmar
seismicHazardFor central Myanmar
lower Myanmar NERFINISHED
separates central lowlands of Myanmar
eastern highlands of Myanmar
tectonicSetting plate boundary between Burma Plate and Sunda Plate

Referenced by (1)

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

Burma Plate associatedWithStructure Sagaing Fault