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, VP=6V_P=6 and VS=3 km/sV_S=3\ \text{km/s}. Find the delay and conditional range.

A Twenty-Second Interval Across Midnight

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Derive the S-P Multiplier from Two Speeds

Assume a common straight path, VP=6V_P=6 and VS=3.5 km/sV_S=3.5\ \text{km/s}, and an S-P delay of 10 s10\ \text{s}. Find the path length and check both travel durations.

Different Travel Times over One Path

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Convert a Source Path to an Epicentral Radius

A surface station has a conditional straight source path of 50 km50\ \text{km}. The assumed focus is 30 km30\ \text{km} below the common station surface. Find horizontal distance.

Depth Correction for a 50-Kilometre Path

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Predict a Conditional S Arrival from Geometry

In the same homogeneous model, a station is 60 km60\ \text{km} horizontally from the epicenter and the source depth is 45 km45\ \text{km}. Let VP=6V_P=6, VS=3 km/sV_S=3\ \text{km/s}. If P arrives at 14:30:00, find the conditional S arrival.

Recover the Sloping Path before the Arrival Difference

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Reject an Impossible Depth and Arrival Pair

An S-P pick gives 3 s3\ \text{s} with VP=6V_P=6, VS=3 km/sV_S=3\ \text{km/s}. A separate interpretation assumes source depth 30 km30\ \text{km}. Can these inputs define a horizontal circle?

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Solve Three Consistent Horizontal Ranges

In local east/north kilometres, stations are A(0,0)A(0,0), B(72,0)B(72,0) and C(0,96)C(0,96). Each inferred horizontal radius is 60 km60\ \text{km}. Find and verify the candidate shown in the left panel.

A Circle Candidate Must Satisfy Original Ranges

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Detect an Algebraic Candidate That Fits No Circle

Keep the same stations, but set all three horizontal radii to 30 km30\ \text{km}. A subtraction calculation still returns (36,48) km(36,48)\ \text{km}. Interpret the right panel of the paired figure.

Check the Inconsistent Right-Hand Case

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Propagate a Timing Bound through the Depth Correction

Assume VP=6V_P=6, VS=3 km/sV_S=3\ \text{km/s} and fixed depth 45 km45\ \text{km}. An S-P delay is 10.0±0.2 s10.0\pm0.2\ \text{s}. Find the corresponding horizontal range interval, considering only this supplied timing bound.

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Compute Seismic Moment with Compatible Area Units

An idealized slipping fault patch is 55 by 4 km4\ \text{km} in its own plane, with uniform shear modulus 30 GPa30\ \text{GPa} and mean slip 0.50 m0.50\ \text{m}. Find scalar moment and MwM_w using the SI constant 9.19.1.

Slipping Fault Area Is Not a Map Footprint

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Keep Moment, Approximate Energy and Local Amplitude Ratios Separate

Compare moment magnitudes 55 and 77. 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?

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Calculate Force Only for a Stated Rigid-Mass Limit

An ideal 50,000 kg50{,}000\ \text{kg} mass is rigidly attached to a base and follows its horizontal acceleration. The chosen ground component has PGA 0.40g0.40g, with g=9.81 m/s2g=9.81\ \text{m/s}^2. Neglect vertical acceleration. Find peak horizontal force magnitude.

A Rigidly Attached Mass Follows the Prescribed Base

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Compare Displacement from Two Supplied PSA Ordinates

Use the synthetic 5%-damped spectral chart. Oscillator A has Tn=0.50 sT_n=0.50\ \text{s} and PSA 0.80g0.80g; oscillator B has Tn=1.00 sT_n=1.00\ \text{s} and PSA 0.40g0.40g. Find each peak relative displacement with g=9.81 m/s2g=9.81\ \text{m/s}^2.

Use the Correct Period and Response Measure

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Read Period-Dependent Site Ratios in a Basin Study

A synthetic study supplies the lesson's 5%-damped PSA comparisons. At 0.2 s0.2\ \text{s} the rock/soil values are 0.30/0.24g0.30/0.24g; at 1.0 s1.0\ \text{s} they are 0.20/0.50g0.20/0.50g. Can one three-to-five amplification factor describe these data?

The Same Site Comparison Can Reverse with Period

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Assess a Partial Pore-Pressure Rise without Declaring Failure

At a point in a reclaimed-land teaching model, hold total vertical stress at 160 kPa160\ \text{kPa}. Initial pore pressure is 120 kPa120\ \text{kPa} and a supplied excess rise is 25 kPa25\ \text{kPa}. Find effective stresses and rur_u, then state what remains unresolved.

Pressure Rise Reduces the Effective-Stress Share

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