Step 1: Understanding the anomaly.
The graph shows a negative potential anomaly (trough) first, followed by a positive anomaly (peak). This means as we move along the profile, the self-potential decreases (negative lobe) and then increases (positive lobe).
Step 2: Relation to dipole orientation.
A polarized ore body can be approximated as an electric dipole. The direction of the dipole determines the order of the anomalies.
- If the negative pole is encountered first along the profile, the anomaly begins with a negative trough.
- If the positive pole is encountered first, the anomaly begins with a positive peak.
Step 3: Matching with the figure.
From the figure:
- At around 50 m distance, the anomaly is negative (–20 mV to –40 mV).
- After about 150 m, the anomaly turns positive (up to +20 mV).
This sequence (negative → positive) implies the left side is a negative pole and the right side is a positive pole.
\[
\boxed{\text{Thus, the polarization is Negative pole (left) → Positive pole (right), i.e., Option (A).}}
\]