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geophysics-expert

Expert-level geophysics covering seismic methods, gravity and magnetics, electromagnetic methods, heat flow, Earth structure, and exploration geophysics.

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Geophysics Expert

Before Starting

  1. Solid Earth or exploration geophysics?
  2. Which method? (seismic, gravity, EM, MT)
  3. Forward modeling or inversion?

Core Expertise Areas

Earth Structure

Crust: continental (35 km avg, granitic) and oceanic (7 km, basaltic). Mantle: upper (solid, peridotite) and lower, separated by transition zone. Core: outer (liquid iron-nickel, generates magnetic field) and inner (solid). Seismic discontinuities: Moho (crust-mantle), 410 and 660 km (phase transitions).

Seismic Methods

Body waves: P-waves (compressional) and S-waves (shear, not through liquids). Surface waves: Rayleigh and Love waves, dispersive, used for shallow structure. Reflection seismics: record reflections from interfaces, used in exploration. Refraction seismics: first arrivals, velocity structure, shallow applications. Tomography: 3D velocity models from travel time inversions.

Gravity and Magnetics

Gravity anomaly: deviation from reference ellipsoid after corrections. Bouguer correction: removes effect of topographic mass. Magnetic anomaly: deviation from IGRF reference field. Magnetic reversals: polarity chrons used for seafloor spreading rate dating.

Electromagnetic Methods

Resistivity: measures electrical resistance of subsurface. MT: magnetotellurics — natural EM fields probe deep conductivity structure. GPR: ground-penetrating radar, high resolution shallow imaging. EM induction: frequency-domain and time-domain methods for conductors.

Best Practices

  • Apply all necessary corrections before interpreting data
  • Integrate multiple methods to reduce non-uniqueness
  • Constrain inversions with geological information
  • Assess uncertainty in all geophysical models

Common Pitfalls

PitfallFix
Non-uniqueness in inversionsUse multiple methods and geological constraints
Missing terrain correctionsAlways apply free-air and Bouguer corrections
Confusing P and S wave arrivalsUse polarization analysis and moveout patterns
Static corrections in reflection seismicApply datum and refraction statics

Related Skills

  • geology-expert
  • seismology-expert
  • physics/fluid-physics-expert

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