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Geophysics

Applied Geophysics: Gravity & Seismics

Gravity corrections, seismic refraction and resistivity — the field methods that image the subsurface without drilling.

PART 1

Topic Breakdown & Traps

The Engineering Principle

Geophysics infers subsurface structure from physical fields. In gravity surveying, raw readings are reduced with the free-air ( mGal) and Bouguer ( mGal) corrections; the residual Bouguer anomaly maps density contrasts (positive over dense bodies). In seismic refraction, energy critically refracts when ; layer depth comes from the intercept time or crossover distance. Electrical resistivity (Wenner array) gives apparent resistivity .

The Core Formula Matrix

Free-air correction: mGal ( in m).

Bouguer correction: mGal ( in g/cm³).

Critical angle: .

Refractor depth: .

Wenner resistivity: .

The ‘IIT Traps’

  • Free-air vs Bouguer. Free-air corrects for elevation only; Bouguer also removes the rock slab's mass.
  • **Critical angle needs .** Refraction surveys require velocity increasing with depth.
  • P faster than S. P-waves arrive first; always.

📚 Standard references

  • An Introduction to Geophysical ExplorationKearey, Brooks & Hill
  • Applied GeophysicsTelford, Geldart & Sheriff
PART 2

Progressive 3-Tier Question Suite

Q1BASIC1 Mark · MCQ
The seismic body wave that is fastest and arrives first is the
Q2MEDIUM2 Marks · NAT
A gravity station sits m above the datum. The free-air correction is _____ mGal.
mGal
Q3HARD2 Marks · NAT
A refraction survey has and m/s. The critical angle is _____ degrees.
°