STUDY OF SEISMIC CONVENTIONAL AND CRS METHOD AT THE STEEP DIP REFLECTOR APPROACH USING SPATIAL GEOMETRY
In the process imagging seismic, reflector slope should be calculated, because Reflections on the field boundary layer which has a slope (dip) in a CMP gather have varying reflection point (smearing). This resulted in artificiality reflector positions represented by the peak point of epic hyperbole....
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Format: | Final Project |
Language: | Indonesia |
Online Access: | https://digilib.itb.ac.id/gdl/view/21260 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |