Seismology intro1 Flashcards
Seismology
Elastic rebound theory (forces bend till breaking point)
Seismic waves are
elastic waves
2 body waves
so called bcs they travel through earth ( P and S)
P
primary (compression) constant compression and dilation
S
secondary or shear, material is shearing it, moves in actualy wave like motion
which wave arrives at station first?
Since Vp > Vs > Vsw P waves generally arrive at a station first
followed by S waves
when P waves hit an interface
P waves hitting an interface at an angle will produce reflected and refracted (transmitted) S and P waves.
Impedance Z
Sign and amplitude of reflected and transmitted wave depends on the “impedance”,
calculating impedence
The impedance, Z, of a layer (or material) is the product of its density and velocity .
impedence contrast
High impedence contrast favours reflection, low impedence contrast favours transmission.
Shadowzone P wave
P-wave SZ is between 104° and 140°.
Shadowzone S wave
S-wave SZ between 104 ° and 256
PREM
Preliminary reference earth model
reference model for earth
gives us velocitys, densitys and other parameters for earth
pressure
Pressure= force / area
can model pressure setting using machines, morphing minerals etc, using phase diagrams to model situations