| Finite element modelling of IP anomalous effect from bodies of any shape located in rugged relief area | Alfred FRASHERI, Neki FRASHERI | 3–6 |
| Estimation of the natural radioactivity of the Albanian clays | Anastas DODONA | 7–12 |
| Temperature dependence of the electrical conductivity of granite and quartz-monzonite from south Bulgaria: Geodynamic inferences | Stefan SHANOV, Yotzo YANEV, Marcela LASTOVICKOVA | 13–19 |
| The effect of the initial earthquake phase shift on the inversion of regional surface wave recordings for the estimation of crustal structure | Özcan ÇAKİR, Salih LİVAOĞLU, Murat ERDURAN | 20–36 |
| Interpretation of gravity and aeromagnetic anomalies of the Konya Region, South Central Turkey | A. ATEŞ, P. KEAREY | 37–44 |
| Maglodan project: The first step in merging the national geomagnetic maps of Romania, Ukraine and the Republic of Moldova | L. BESUTIU, I. PASHKEVICH, G. BESUTIU, V. NEAGA, M. IVAN | 45–52 |
| Separation of magnetic fields in geophysical studies using a 2-D multi-resolution wavelet analysis approach | Osman N. UÇAN, Serhat SEKER, A. Muhittin ALBORA, Atilla ÖZMEN | 53–58 |
| Investigation of protential fields anomalies related with the Philippi basin and granitoid intrusion, NE Greece | A. STAMPOLIDIS, G. N. TSOKAS, G. ELEFTERIADIS, D. KONDOPOULOU | 59–66 |
| Archaeointensity results from two ceramic kilns from N. Greece | V. SPATHARAS, G. N. TSOKAS, D. KONDOPOULOU, I. LIRITZIS | 67–72 |
| Influence of the geomagnetic activity on the human functional systems | Irina STOILOVA, Thomas ZDRAVEV | 73–76 |
| The Milos Island bouguer anolmaly revisited by means of a complex attribute analysis and inferred source parameter estimates | G. N. TSOKAS | 77–86 |
| Analysis of geomagnetic field anomalies in the Leptokarya area, NE Greece | A. STAMPOLIDIS, G. N. TSOKAS, D. KONDOPOULOU, D. PANAGIOTOPOULOS, A. SAVVAIDIS | 87–92 |