Seismic Reflection Surveying Using the figure to the left, compute reflection coefficient and transmission coefficients across the boundary if the density of layer 1 is set to 1.0 g/cm and the density of layer 2 is 2.4 g/cm. Compute also the maximum normal move out (ie. Boat Sea Surface the difference between maximum travel time recorded and a zero-offset case) for the Source reflection events from the seafloor. Assume the distance
Seismic Reflection Surveying Using the figure to the left, compute reflection coefficient and transmission coefficients across the boundary if the density of layer 1 is set to 1.0 g/cm and the density of layer 2 is 2.4 g/cm. Compute also the maximum normal move out (ie. Boat Sea Surface the difference between maximum travel time recorded and a zero-offset case) for the Source reflection events from the seafloor. Assume the distance
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Transcribed Image Text:Seismic Reflection Surveying t
Using the figure to the left, compute reflection coefficient and transmission coefficients across the boundary if the
density of layer 1 is set to 1.0
g/cm and the density of layer 2
is 24g/an'. Compute also the
maximum ormal move out (Le.
Bost
Sea Surface
the difference between
maximum travel time recorded
and a zero-offset case) for the
reflection events from the
Soutce
Layer 1 (water).
V= 1500m/s
seafloor, Assume the distance
2000 m between two consecutive
geophones of 50 m.
Layer 2
V = 2000m/s
500 m
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