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MIYASHIRO, A. (1955); Pyralpsite garnets in volcanic rocks. - J. Geol. Soc. Japan, J51: 463-470. NAGY, G. (1975): Temperature determination of igneous processes on the basis of the composition of coexistent mineral pairs. - Acta geol. hung., 1_9: 43-58. NOSKE-FAZEKAS, G. (1980): Statistical investigations of plagioclase twin laws in lavas erupted between the Danube and the Central Börzsöny Mountains (Hungary). - Annls hist.-nat. Mus. natn. hung., 72: 11-18. NOSKE-FAZEKAS, G. & EMBEY-ISZTIN, A. (1978): New data to the mineralogy of the basic intrusion around the Village Szarvaskő, Hungary. - Annls hist. - nat. Mus. natn. hung., J_0: 13-25. OLIVER, R. L. (1956): The origin of garnets in the Borrowdale Volcanic Series and asso­ciated rocks, English Lake District. - Geol. Mag., _93: 121-139. PANTO, Gy. (1970): A Börzsöny hegység északi részének harmadidőszaki vulkanizmusa. [Cenozoic volcanism in the northern part of the Börzsöny Mts.J - Budapest, 302 pp (in Hungarian). PERRIN, R. & ROUBAULT, M. (1949): Des eriteres permattant de determiner le mode de formation des filons a bords paralleles: injection ou remplacement. - Bull. Soc. Géol. Fr. , 19: 614-656. STERN, CR. & WYLLIE, P. J. (1978): Phase compositions through crystallization inter­vals in basalt-andesite-H O at 30 kbar with implications for subduction zone mag­mas. - Am. Min., 63: 641-663. SZENTPÉTER Y, Zs. (1 953): A déli Bükkhegység diabáz és gabbró-tömege (The diabase and gabbro masses of the Southern Bükk Mts. ) - Magy. Ali. Földt. Int. Evk. , 41 ; 3-92. TÓTH, M. (1882): Magyarország ásványai (Minerals of Hungary) - Budapest, 565 pp. WELLS, A. K. & BISHOP, A.C. (1954): The origin of aphtes. - Proc. Geol. Assoc., _65: 95-114. ' ZIPSER, C.A. (1817): Versuch eines topographisch-mineralogischen Handbuches von Un­garn. - Oedenburg, XXXI + 440 pp. Authors' address: Dr. Antal EMBEY-ISZTIN Dr. Gabriella NOSKE-FAZEKAS Department of Mineralogy and Petrology Hungarian Natural History Museum H-1088 Budapest Múzeum körút 14-16. Hungary EXPLANATION TO PLATES PLATE I Fig. Fig. 1 2 Plagioclase corona around ruptured garnet. Nagybörzsöny Garnet inclusion in a biotite crystal, Bányabérc PLATE II Fig. Fig. 1 2 Plagioclase in contact with garnet. Pilisszentlélek Flow lines around a garnet crystal. Pilisszentlélek PLATE III Fig. Fig. 1 2 Inclusion-rich ruptured garnet, Nagybörzsöny Unfractured inclusion-poor garnet. Pilisszentlélek

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