Seismic Wave Velocity in Various Rock Types
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The seismic waves produced by the detonation of an explosive charge or any other system are transmitted through the Earth in the form of vibrations or waves that travel at different speeds. These speeds are influenced by several factors, including lithology, depth, porosity of the material, compaction, lithification, and fluid content, among others. Furthermore, these speeds depend on the elastic modulus and density. These parameters are essential for velocity analysis in the interpretation of seismic data. Below is a table showing the propagation speeds of seismic waves; these values specifically refer to longitudinal waves (P-waves).
| Material | Velocity (V) [m/s] |
|---|---|
| Weathering layer | 300–900 |
| Modern alluvium | 350–1,500 |
| Clays | 1,000–2,000 |
| Marls | 1,800–3, |