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Átúr, Bratislava, Slovakia \n Institute of Nuclear Research, Hungarian Academy of Sciences, Debrecen, Hungary \n Faculty of Mineral Resources, North University, Baia Mare, Romania \n Cited By :65 \n Export Date: 21 June 2021 \n Correspondence Address: Lexa, J.; Geological Institute, , Bratislava, Slovakia \n Funding details: Hungarian Scientific Research Fund, OTKA, K 68153 \n Funding details: Vedecká Grantová Agentúra MŠVVaŠ SR a SAV, VEGA, 2/0171/08 \n Funding text 1: This paper is to be presented in the XIX Congress of the Carpathian Balkan Geological Association in Thessaloniki on September 23–26, 2010. To attend the XIX CBGA congress, JL was invited by the Organizing Committee of the Congress, KN was supported by the Massey University Leave & Ancillary Appointments Committee granted fund (LAAC10/37). IS thanks the Institute of Geodynamics, Romanian Academy and the Organizing Committee of the Congress for support. ZP acknowledge the financial support provided by the Hungarian national Scientific Fund (OTKA No. K 68153). JL acknowledges support of the VEGA grant 2/0171/08. Constructive comments by anonymous journal reviewers and Managing Editor, Katarzyna Cyran helped to improve the quality of the manuscript.\nFunding Agency and Grant Number: Massey University Leave & Ancillary Appointments Committee granted fund [LAAC10/37]; Institute of Geodynamics, Romanian Academy; Organizing Committee of the Congress; Hungarian national Scientific Fund (OTKA)Orszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [K 68153]; VEGAVedecka grantova agentura MSVVaS SR a SAV (VEGA)European Commission [2/0171/08]\n Funding text: This paper is to be presented in the XIX Congress of the Carpathian Balkan Geological Association in Thessaloniki on September 23-26, 2010. To attend the XIX CBGA congress, JL was invited by the Organizing Committee of the Congress, KN was supported by the Massey University Leave & Ancillary Appointments Committee granted fund (LAAC10/37). IS thanks the Institute of Geodynamics, Romanian Academy and the Organizing Committee of the Congress for support. ZP acknowledge the financial support provided by the Hungarian national Scientific Fund (OTKA No. K 68153). JL acknowledges support of the VEGA grant 2/0171/08. 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It shows a diverse compositional variation in response to a complex interplay of subduction with roll-back, back-arc extension, collision, slab break-off, delamination, strike-slip tectonics and microplate rotations, as well as in response to further evolution of magmas in the crustal environment by processes of differentiation, crustal contamination, anatexis and magma mixing. Since most of the primary volcanic forms have been affected by erosion, especially in areas of post-volcanic uplift, based on the level of erosion we distinguish: (1) areas eroded to the basement level, where paleovolcanic reconstruction is not possible; (2) deeply eroded volcanic forms with secondary morphology and possible paleovolcanic reconstruction; (3) eroded volcanic forms with remnants of original morphology preserved; and (4) the least eroded volcanic forms with original morphology quite well preserved. The large variety of volcanic forms present in the area can be grouped in a) monogenetic volcanoes and b) polygenetic volcanoes and their subsurface/intrusive counterparts that belong to various rock series found in the CPR such as calc-alkaline magmatic rock-types (felsic, intermediate and mafic varieties) and alkalic types including K-alkalic, shoshonitic, ultrapotassic and Na-alkalic. The following volcanic/subvolcanic forms have been identified: (i) domes, shield volcanoes, effusive cones, pyroclastic cones, stratovolcanoes and calderas with associated intrusive bodies for intermediate and basic calc-alkaline volcanism; (ii) domes, calderas and ignimbrite/ash-flow fields for felsic calc-alkaline volcanism and (iii) dome flows, shield volcanoes, maars, tuffcone/tuff-rings, scoria-cones with or without related lava flow/field and their erosional or subsurface forms (necks/ plugs, dykes, shallow intrusions, diatreme, lava lake) for various types of K- and Na-alkalic and ultrapotassic magmatism. 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