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Offset ,[object Object]
Acoustic Impedance   ,[object Object]
Seismogram   ,[object Object]
Seismograph   ,[object Object]
 
Geophone   ,[object Object]
 
Seabed Geophone ,[object Object]
Hydrophone ,[object Object],[object Object]
 
Takeout on Seismic Cable
Streamer   ,[object Object]
 
Multiplex ,[object Object]
Binary and Decimal Amplitude
Air Gun ,[object Object]
[object Object]
 
Vibrator   ,[object Object],[object Object]
 
[object Object]
 
Frequency
Wavelength
Amplitude
[object Object],[object Object],[object Object],[object Object],[object Object]
 
Correlation ,[object Object]
Signal ,[object Object]
Noise ,[object Object]
Coherent Noise ,[object Object]
Random Noise ,[object Object]
Ground Roll ,[object Object]
 
Signal-to-Noise ratio   ,[object Object]
Multifold Fold CMP Coverage
If there are N geophones and the array moves forward a distance of nΔx between shots, it can be shown that the number of rays that share the same common midpoint is  N/2n . This is the fold of the data. Fold is sometimes reported as a percentage of coverage (100×N/2n %) In the example below, there are 6 geophones and the array moves forward a distance of 1Δx between shots. This gives 3-fold CMP coverage or 300% coverage.
 
Marine Seismic Acquisition ,[object Object]
 
VSP ,[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
 
check-shot survey ,[object Object]
 
Synthetic Seismogram ,[object Object]
Synthetic Seismogram
The synthetic seismogram in the fifth column was generated by convolving the digitized sonic and density logs with a wavelet shown in the column to the right. By comparing geological markers picked on logs, such as the top of the chalk in this display, with major reflections on the seismic section, seismic data can be used to map physical properties between wells.
 
[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Zero-Phase Wavelet ,[object Object]
One-Dimensional Seismic Data ,[object Object],[object Object],[object Object]
Two-Dimensional Seismic Data ,[object Object]
Diagram of a Two-Dimensional seismic survey   ,[object Object]
 
Concept of 3D ,[object Object],[object Object],[object Object]
In-Line ,[object Object]
Cross-Line ,[object Object]
The crosslines of a 3D survey are perpendicular to the direction in which the data were acquired. The in-lines of a 3D survey are parallel to the direction in which the data were acquired, or in marine data, the direction in which the boat moves.
Bin ,[object Object],[object Object],[object Object]
Three-Dimensional Seismic Data ,[object Object],[object Object]
3D Seismic
 
 
 
 
 
WHY WE NEED 3-D? ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
3-D Advantages ,[object Object],[object Object],[object Object],[object Object],[object Object]
 
Swath Method ,[object Object]
4D Seismic ,[object Object]
 
[object Object]
3C Seismic Data ,[object Object]
4C Seismic ,[object Object]
Obtaining four-component seismic data using a multiwave array system. Each sensor station within the cable comprises one hydrophone and three orthogonally oriented geophones to record both pressure and particle velocity.
Need of Multi-Component Data   ,[object Object],[object Object],[object Object],[object Object],[object Object]
Unconformity A geological surface separating older from younger rocks and representing a gap in the geologic record. Such a surface might result from a hiatus in deposition of sediments, possibly in combination with erosion, or deformation such as faulting.
Angular Unconformity: A surface that separates younger strata from eroded, dipping, older strata and represents a gap in the geologic record.
 
 
 
 
 
 
 
 
 
 
Fault plane is oriented between 30 and 90 degrees (measured from horizontal)
Fault plane is at less than 30 degrees
Fault plane is oriented between 30 and 90 degrees (measured from horizontal)
Fault plane is at less than 30 degrees
 
 
  Pinch-out   A  type of stratigraphic trap. The termination by thinning or tapering out ("pinching out") of a reservoir against a nonporous sealing rock creates a favorable geometry to trap hydrocarbons, particularly if the adjacent sealing rock is a source rock such as a shale.
Reef ,[object Object]
First Break   ,[object Object]
First Break
Common Depth Point   ,[object Object]
Common Midpoint   ,[object Object]
[object Object]
Common Depth Point & Common Mid Point
 
Normal Moveout ,[object Object]
[object Object]
Two-Way Traveltime ,[object Object]
Creep ,[object Object]
wavelet   ,[object Object]
[object Object]
spherical wave ,[object Object]
Blowout   ,[object Object]
shadow zone   ,[object Object]
 
Epicenter, Hypocenter and Focucs ,[object Object]
Critical Angle ,[object Object]
Critical Reflection   ,[object Object]
Channel ,[object Object]
Exploratory Well  ,[object Object]
Appraisal Well ,[object Object],[object Object],[object Object]
Development Well ,[object Object],[object Object],[object Object]
Production Well ,[object Object]
Root-mean-square Velocity ,[object Object]
Average Velocity   ,[object Object]
Anisotropy - isotropy comparison ,[object Object]
Multiple Reflection   ,[object Object]
[object Object]
Long-path multiple ,[object Object]
[object Object]
Short-path Multiple ,[object Object]
Ghost ,[object Object]
[object Object]
Primary Reflection   ,[object Object]
[object Object]
Peg Leg Multiples ,[object Object]
 
 
Up, Middle & Down Stream Activities ,[object Object]
Christmas Tree ,[object Object]
Seismometer ,[object Object]
lithosphere   ,[object Object]
Asthenosphere   ,[object Object]
Automatic Gain Control   ,[object Object]
Uphole Survey ,[object Object]

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Some basic concepts

  • 1.
  • 2.
  • 3.
  • 4.
  • 5.  
  • 6.
  • 7.  
  • 8.
  • 9.
  • 10.  
  • 12.
  • 13.  
  • 14.
  • 15. Binary and Decimal Amplitude
  • 16.
  • 17.
  • 18.  
  • 19.
  • 20.  
  • 21.
  • 22.  
  • 26.
  • 27.  
  • 28.
  • 29.
  • 30.
  • 31.
  • 32.
  • 33.
  • 34.  
  • 35.
  • 36. Multifold Fold CMP Coverage
  • 37. If there are N geophones and the array moves forward a distance of nΔx between shots, it can be shown that the number of rays that share the same common midpoint is N/2n . This is the fold of the data. Fold is sometimes reported as a percentage of coverage (100×N/2n %) In the example below, there are 6 geophones and the array moves forward a distance of 1Δx between shots. This gives 3-fold CMP coverage or 300% coverage.
  • 38.  
  • 39.
  • 40.  
  • 41.
  • 42.
  • 43.  
  • 44.
  • 45.  
  • 46.
  • 48. The synthetic seismogram in the fifth column was generated by convolving the digitized sonic and density logs with a wavelet shown in the column to the right. By comparing geological markers picked on logs, such as the top of the chalk in this display, with major reflections on the seismic section, seismic data can be used to map physical properties between wells.
  • 49.  
  • 50.
  • 51.
  • 52.
  • 53.
  • 54.
  • 55.
  • 56.  
  • 57.
  • 58.
  • 59.
  • 60. The crosslines of a 3D survey are perpendicular to the direction in which the data were acquired. The in-lines of a 3D survey are parallel to the direction in which the data were acquired, or in marine data, the direction in which the boat moves.
  • 61.
  • 62.
  • 64.  
  • 65.  
  • 66.  
  • 67.  
  • 68.  
  • 69.
  • 70.
  • 71.  
  • 72.
  • 73.
  • 74.  
  • 75.
  • 76.
  • 77.
  • 78. Obtaining four-component seismic data using a multiwave array system. Each sensor station within the cable comprises one hydrophone and three orthogonally oriented geophones to record both pressure and particle velocity.
  • 79.
  • 80. Unconformity A geological surface separating older from younger rocks and representing a gap in the geologic record. Such a surface might result from a hiatus in deposition of sediments, possibly in combination with erosion, or deformation such as faulting.
  • 81. Angular Unconformity: A surface that separates younger strata from eroded, dipping, older strata and represents a gap in the geologic record.
  • 82.  
  • 83.  
  • 84.  
  • 85.  
  • 86.  
  • 87.  
  • 88.  
  • 89.  
  • 90.  
  • 91.  
  • 92. Fault plane is oriented between 30 and 90 degrees (measured from horizontal)
  • 93. Fault plane is at less than 30 degrees
  • 94. Fault plane is oriented between 30 and 90 degrees (measured from horizontal)
  • 95. Fault plane is at less than 30 degrees
  • 96.  
  • 97.  
  • 98. Pinch-out A type of stratigraphic trap. The termination by thinning or tapering out ("pinching out") of a reservoir against a nonporous sealing rock creates a favorable geometry to trap hydrocarbons, particularly if the adjacent sealing rock is a source rock such as a shale.
  • 99.
  • 100.
  • 102.
  • 103.
  • 104.
  • 105. Common Depth Point & Common Mid Point
  • 106.  
  • 107.
  • 108.
  • 109.
  • 110.
  • 111.
  • 112.
  • 113.
  • 114.
  • 115.
  • 116.  
  • 117.
  • 118.
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  • 128.
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  • 131.
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  • 136.
  • 137.
  • 138.  
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  • 140.
  • 141.
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  • 143.
  • 144.
  • 145.
  • 146.