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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: .
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 Exploration — Kearey, Brooks & Hill
- Applied Geophysics — Telford, 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.
°