Pit N Thesis · thesis-4-32
Electrofacies — B2–C interburden
In the thesis correlation, the B2–C is bounded by coal markers already identified in core. The irregular gamma motif is consistent with the observed alternation—the b2–c interburden is dominated by very fine sandstone and siltstone—but the curve is an averaged petrophysical response rather than a facies name.
SOURCE-LED TECHNICAL READING
Geological interpretation and evidential boundary
In the thesis correlation, the B2–C is bounded by coal markers already identified in core. The irregular gamma motif is consistent with the observed alternation—the b2–c interburden is dominated by very fine sandstone and siltstone—but the curve is an averaged petrophysical response rather than a facies name. The interpretation is retained only where the depth match, density track, recovery record and neighbouring wells exclude a simpler logging or sampling explanation. The corresponding internship figure is the same record in an earlier report context, not independent confirmation.
- Source
- Private thesis source vault · Chapter IV record
- Location in source
- PDF page 133
- Image quality
- Source scan
- Record ID
- thesis-4-32
