Seismology: Worked Applications
All observations, specimens, spectra and stations below are synthetic teaching data. State the source/path model and units before interpreting a result.
S-P Clock Difference Across Midnight
A station records P at 23:59:50 and S at 00:00:10 the next day. In a homogeneous, zero-depth teaching model, and . Find the delay and conditional range.
Step-by-Step Solution
0 of 3 Steps CompletedDerive the S-P Multiplier from Two Speeds
Assume a common straight path, and , and an S-P delay of . Find the path length and check both travel durations.
Step-by-Step Solution
0 of 2 Steps CompletedConvert a Source Path to an Epicentral Radius
A surface station has a conditional straight source path of . The assumed focus is below the common station surface. Find horizontal distance.
Step-by-Step Solution
0 of 2 Steps CompletedPredict a Conditional S Arrival from Geometry
In the same homogeneous model, a station is horizontally from the epicenter and the source depth is . Let , . If P arrives at 14:30:00, find the conditional S arrival.
Step-by-Step Solution
0 of 3 Steps CompletedReject an Impossible Depth and Arrival Pair
An S-P pick gives with , . A separate interpretation assumes source depth . Can these inputs define a horizontal circle?
Step-by-Step Solution
0 of 3 Steps CompletedSolve Three Consistent Horizontal Ranges
In local east/north kilometres, stations are , and . Each inferred horizontal radius is . Find and verify the candidate shown in the left panel.
Step-by-Step Solution
0 of 2 Steps CompletedDetect an Algebraic Candidate That Fits No Circle
Keep the same stations, but set all three horizontal radii to . A subtraction calculation still returns . Interpret the right panel of the paired figure.
Step-by-Step Solution
0 of 3 Steps CompletedPropagate a Timing Bound through the Depth Correction
Assume , and fixed depth . An S-P delay is . Find the corresponding horizontal range interval, considering only this supplied timing bound.
Step-by-Step Solution
0 of 3 Steps CompletedCompute Seismic Moment with Compatible Area Units
An idealized slipping fault patch is by in its own plane, with uniform shear modulus and mean slip . Find scalar moment and using the SI constant .
Step-by-Step Solution
0 of 3 Steps CompletedKeep Moment, Approximate Energy and Local Amplitude Ratios Separate
Compare moment magnitudes and . Separately compare two calibrated local-amplitude magnitudes differing by two units at identical distance/instrument correction. What ratios follow, and what site motion remains unknown?
Step-by-Step Solution
0 of 3 Steps CompletedCalculate Force Only for a Stated Rigid-Mass Limit
An ideal mass is rigidly attached to a base and follows its horizontal acceleration. The chosen ground component has PGA , with . Neglect vertical acceleration. Find peak horizontal force magnitude.
Step-by-Step Solution
0 of 3 Steps CompletedCompare Displacement from Two Supplied PSA Ordinates
Use the synthetic 5%-damped spectral chart. Oscillator A has and PSA ; oscillator B has and PSA . Find each peak relative displacement with .
Step-by-Step Solution
0 of 2 Steps CompletedRead Period-Dependent Site Ratios in a Basin Study
A synthetic study supplies the lesson's 5%-damped PSA comparisons. At the rock/soil values are ; at they are . Can one three-to-five amplification factor describe these data?
Step-by-Step Solution
0 of 3 Steps CompletedAssess a Partial Pore-Pressure Rise without Declaring Failure
At a point in a reclaimed-land teaching model, hold total vertical stress at . Initial pore pressure is and a supplied excess rise is . Find effective stresses and , then state what remains unresolved.