Mapa mental
Lect 11: Stacking

Contenido del mapa
Lect 11: Stacking
Where did it come from??
- Pre-Stack Time Migration
- After Migration section
- Post- Stack Time Migration
- Before Migration section
- Pre-Stack Time Migration
2 Types of Stacking Process:
- Horizontal Stacking : Stack in horizontal direction by sum of the NMO corrected data
- NMO corrected data that obtain from velocity analysis being use for the horizontal
- Vertical Stacking: Add & average the seismic record over same shot position
- Stack on a particular seismic trace. (Rarely use - as will not give clear representative of subsurface)
- Horizontal Stacking : Stack in horizontal direction by sum of the NMO corrected data
The result is an approximation of a zero-offset section, where reflections come from below the CMP postion
Objectives of Stacking process:
- A true representation of Earth's subsurface
- Improve Signal-to-Noise ratio
- Attenuate multiples
- Reduce data volume
Stacking Method
- Mean Stack
- All NMO-corrected traces are summed and divided by the number of traces:
- Weighted Stack
- Unequal weighting of the traces
- May yield better results.
- Suitable for traces contain a lot of noise
- Often used to suppress multiples
- Need to introduce a weight factor.
- Most use in industry
- Diversity stacking / Min-Max-exclude (rarely use)
- Certain traces are muted and not included in the stacking procedure
- When certain values differ too much from the average value they can be muted (diversity stacking). this to reduce the influence of spikes
- Exclusion of traces with the minimum and maximum amplitudes in the stacking procedure (min-max-exclusion or alpha-trimmed stack)
- Mean Stack
Effect of Velocity
- NMO V: 1700 m/s good stack response
- NMO V: 1500 m/s event overcorrected poor stack response
- NMO V: 2000 m/s event undercorrected poor stack response
Imágenes y archivos del mapa
Información
- Descripción
- Mapa Mental sobre Lect 11: Stacking, creado por Nur Nazihah el 18/07/2018.
- Creado por
- Nur Nazihah
- Visitas
- 0
- Valoración




