Table 1 Optimal parameters for identifying river channel boundaries in the study area.

From: Research and application of 3D attribute fusion technology based on lithology probability analysis

Option

Parameter

River channel boundary detection

Noise attenuation

Computation speed

Number of Seismic Traces

2

Best

-

Fast

4

Better

-

Medium

8

Good

-

Slow

Dip Angle

0°

Poor

-

Fast

10°

Good

-

Slow

20°

Poor

-

Very Slow

Time Window Size

1 ms

Average

Average

Faster

3 ms

Good

Good

Fast

6 ms

Average

Average

Slow

9 ms

Average

Average

Very Slow