Seismology
Seismic reflection is a geophysical method used to investigate subsurface geological structures by analyzing the reflected seismic waves from layers of rock or sediment. This technique relies on sending seismic waves into the ground and measuring the time it takes for them to bounce back after hitting different layers, providing insights into the Earth's composition and fault systems. The ability to distinguish between various rock types and identify fault geometries plays a critical role in understanding earthquake source models and is essential in exploration activities for resources like oil and gas.
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