Complexity of S-wave Splitting
Waves sourced by S
1
Waves sourced by S
2
Upper
Anisotropic
Rock
Lag from
lower level
S´
11
S´
12
S´
21
S´
22
Upper natural
coordinate frame
S
1
S
2
Lower
Anisotropic
Rock
S
1
S
2
Converted P to S reflection
Lower natural
coordinate frame
S
1
S
2