lecture 7 Flashcards
subduction zone earthquakes
crustal earthquakes within forearc
megathrust events along shallow plate interface
outer rise normal faults from plate flexure
intermediate depth intraslab events
deep earthquakes within subducting slab
seismicity associate with arc volcanism
megathrust earthquake cycle
earthquake cycle on subduction zone megathrust faults involves vertical and horizontal motions
interseismic period of megathrust
lower plate slowly subducts and is locked
at the trench upper plate is dragged downwards but at the coast it contracts and bulges upwards
coseismic phase of megathrust
motions are reversed, megathrust slips upper plate rebounds and sea-floor trench suddenly uplifted and the coastline subsides
japan trench
earthquake ruptured the japan trench megathrust where pacific plate subducts westward beneath the Japan arc
- range of frictional behaviors that control earthquake depths
conditionally stable
originally thought megathrust was aseismic but it was conditionally stable
- allowed rupture all the way to the trench
continental plate boundary zone
involve upper crustal earthquakes only
- seismogenic zone is like 15km thick
- continental collision zones, shear zones, rifts
arabia eurasia collision
africa arabia and india continental plates are each moving north
results in broad zone of mountain building called alpine himalayan belt
arabia eurasia collision
earthquakes occur along the edges of mountain ranges
- mountains are being raised along thrust faults in response to the collision
bam earthquake
Mw 6.6 - desert city with the largest mud brick building in the world
one of the first mapped using InSAR
InSAR
used to map earthquakes - large antenna stimulated by combining multiple images along track (Synthetic Aperture Radar)
measures amplitude + phase of back scattered energy
bam0baravat ridge
earthquake rupture runs along
- ridge-bounding fault is impermeable so water table dams against it
tunnels called “qanats” tap into this water source
arid regions
active faults act as a water source in arid tectonic landscapes
- many cities situated next to active faults
ex. Tehran
abundance of highly destructive earthquakes within the alpine himalayan belt
intraplate earthquakes
occur far from plate boundaries (unusual)
plates arent rigid and can slowly deform internally
- pose a hazard to central and eastern canada
postglacial earthquakes
postglacial rebound following melting of ice sheets causes crust to flex and triggers postglacial earthquakes