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 rift ⓘ
linked to: Reelfoot fault
partOf New Madrid Seismic Zone ⓘ
reactivatedFrom Paleozoic rift faults ⓘ
relatedTo Mississippi embayment ⓘ
Reelfoot rift margin ⓘ
linked to: Reelfoot fault
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 ⓘ