 The study area is covered by neoproto-rosic heterogeneous collection of aphiolites, island arch assemblages, and intrusions. Airborne magnetic and radiometric data were applied and compared with remote sensing investigations for deciphering the structural and hydrothermal alteration patterns within the study area. The results demonstrated a different extent from one sensor to another, highlighting their varied efficacy in detecting hydrothermal alterations, mainly hydroxyl-bearing alterations and ion oxides. Furthermore, the analysis of airborne magnetic and radiometric data showed hydrothermal alteration zones that are consistent with the detected alteration pattern. The coincidence between high magnetic anomalies, high values of the KF ratio, and the resultant alterations confirms the real alteration anomalies. Overall, the remote sensing results and airborne geophysical indications were verified with fieldwork and petrographic investigations, and strongly recommend combining ASTA and Sentinel-2 results in further investigations.