Seismic Refraction Method, 6
Abstract
It has been seen that I= DELAY SP + DELAY GEOPHONE. Then at a constant close to (DELAY SP) the curve of the intercepts corresponds to the curve DELAY GEOPHONE.
Fields of Study & Subjects
Seismic Imaging and Inversion Techniques
Seismic Waves and Analysis
Geophysical Methods and Applications
Publication details
- Journal / source
- CRC Press eBooks
- Pages
- 390–390
- Publication date
- 12 February 2026
- Language
- EN
- Document type
- Book chapter