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threshold for vertical resolution generally is a quarter of the dominant wavelength (Sheriff, 1994), although this criterion is subjective and depends on the noise level in the data.

      The above criterion implies that the minimum depth separation (Δz) is:

      (2.1.22)equation

      As for the horizontal resolution, instead it refers to how close two reflecting points can be situated horizontally yet be recognized as two separate points rather than one.

Material Type Relative Dielectric Constant εr = ε/ε0 Electrical Conductivityσ (mS/m) EM Waves Velocity V (m/ns) EM Waves Attenuation α (dB/m)
Air 1 0 0.30 0
Distilled water 80 0.01 0.033 2*10−3
Fresh water 80 0.5 0.033 0.1
Salt water 80 3*104 0.01 103
Dry sands 3‐5 0.01 0.15 0.01
Saturated sands 20‐30 0.1‐1 0.06 0.03‐0.3
Limestone 4‐8 0.5‐2 0.12 0.4‐1
Shale 5‐15 1‐100 0.09 1‐100
Silt 5‐30 1‐100 0.07 1‐100
Clay 5‐40 2‐1000 0.06 1‐300
Granite 4‐6 0.01‐1 0.13 0.01‐1
Dry salt 5‐6 0.01‐1 0.13 0.01‐1
Freq. (MHz) P(ns) λ (m) @ v= c λ (m) @ v= (1/3) c λ (m) @ v= (1/6) c
1 1000 300 100 50
10 100 30 10 5
30 33 10 3.3 1.65
100 10 3 1 0.5
300 3.3 10 3.3 1.65
500 2 0.6 0.2 0.1
1000 1 0.3 0.1 0.05
2000 0.5 0.15 0.05 0.025
3000 0.33 0.1 0.03 0.015

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