New Madrid Seismic Zone margin structures

E344944

The New Madrid Seismic Zone margin structures are a set of buried faults and related tectonic features in the central United States that accommodate intraplate deformation and are responsible for the region’s significant earthquake hazard.

All labels observed (1)

Label Occurrences
New Madrid Seismic Zone margin structures canonical 1

How this entity was disambiguated

Statements (47)

Predicate Object
instanceOf fault system
seismogenic structure
tectonic structure set
accommodates intraplate deformation
age Paleozoic basement origin with reactivation in late Cenozoic
associatedWith 1811–1812 New Madrid earthquakes
ground deformation along the Mississippi River
large intraplate earthquakes
subsidence in the Mississippi embayment
buriedUnder Mississippi embayment sediments
characterizedBy blind faults
normal faulting
reverse faulting
strike-slip faulting
controls earthquake hypocenter distribution in the New Madrid Seismic Zone
linear trends of seismicity
deformationStyle compressional reactivation of rift margins
oblique-slip faulting
hasPart Blytheville arch-related faults
Bootheel lineament
Commerce geophysical lineament-related faults
Cottonwood Grove fault zone
Mississippi River Valley graben-bounding faults
Reelfoot fault
hasSeismogenicDepthRange approximately 5–25 km
hasUncertainty poor surface expression due to burial
hazardLevel high for moderate-to-large earthquakes in central United States
influences probabilistic seismic hazard maps for the central United States
locatedIn Arkansas
Illinois
Kentucky
Missouri
Tennessee
central United States
mappedBy aeromagnetic surveys
borehole data
gravity surveys
seismic reflection data
overlies Reelfoot fault
surface form: Reelfoot rift
partOf New Madrid Seismic Zone
reactivatedFrom Paleozoic rift faults
relatedTo Mississippi Embayment
surface form: Mississippi embayment

Reelfoot fault
surface form: Reelfoot rift margin
responsibleFor New Madrid Seismic Zone earthquake hazard
studiedBy United States Geological Survey
studiedFor seismic hazard assessment
tectonicSetting intraplate

How these facts were elicited

Referenced by (1)

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

North American plate boundary system hasPart New Madrid Seismic Zone margin structures