Investigation of potential fields anomalies related with
the Philippi basin and granitoid intrusion, NE Greece

A. Stampolidis, G. N. Tsokas, G. Elefteriadis and D. Kondopoulou

Geophysical Laboratory, Aristotle University of Thessaloniki, 54006, Thessaloniki, Greece

Received 1 November 2000; accepted 15 April 2000

Abstract: Gravity and magnetic data were used in the study of Philippi basin and intrusion. The most rigorous methods were used for the recompilation of the aeromagnetic map of Macedonia and Thrace. Philippi basin has a maximum depth of about 5.4 km. The aeromagnetic data reveal the presence of a large intrusion, much greater than the two small granitic outcrops.

Key Words: Plilippi, Granitoid, Potential Fields, N. Greece