Scientific work in basalt volcanic areas in our area can play an important role in the research of intracontinental / intra-plate monogenetic volcanic fields. Our research group primarily explores the conditions of magma formation, the nature of the source area of magmas, the conditions of deep magma reservoir formation, the rate of magma upflow, the change in magma composition during the construction of a monogenetic volcano, and the associated eruption mechanisms by studying the minerals in basalts in detail. During our investigations, we pay special attention to the latest basalt volcanic eruptions in our region, such as the Persányi basalt volcanic field and the Selmec-Nógrád-Gömör volcanic area. The basalt occurrences of the Bakony-Balaton Uplands and the Kemenesalja provide a great opportunity to study the basalt volcanic function in many ways.
