4. Why Seismic?
• Seismic forms the backbone of hydrocarbon
exploration.
• The predominance over other geophysical
methods is due to:
– High accuracy
– High resolution
– Penetration to a great depth.
8. Fundamentals .....
Geophones record the movement of the ground due to the propagation of
seismic energy as seismograms or seismic traces. Seismograms are frequently
displayed as "wiggle traces."
9. Components of Data Acquisition
• Energy source with adequate power
• Sensors to detect the signal
• Recording instrument to record data
• Positioning (and Navigation)
14. Seismic Survey Methods
• 2D Seismic
• 3D Seismic
• 4D Seismic
• OBC (Ocean Bottom Cable) - can be of any
type like 2D, 3D or 4D
• VSP Survey (bore-hole seismic)
15. 2D Seismic Data Acquisition
Source
Geophones
Seismic Waves
Recording
16. Seismic data is digitally recorded in the field along a predefined line,
using appropriate shot and receiver geometries.
Layer-1
Layer-2
Layer-3
Shots
Receivers
SEISMIC DATA ACQUISITION - 2D
21. Seismic API
Acquisition, Processing & Interpretation
Acquisition:
Acquiring data
Processing:
Correction & enhancement of
Signal to noise
Interpretation:
converting to Geological
meaning