Szekessy Vilmos (szerk.): A Magyar Természettudományi Múzeum évkönyve 56. (Budapest 1964)
Csalogovits, J. I.: The non-magnetic derivation of Atlantic and Mediterranean rock-provinces and their connection with orogenic metamorphism
effect (FENNER, BARTH, SZÁDECKY-KARDOSS) do not cause alkalinization; only the primary chlorite formation brought about by the increase of water contents may result in such an equilibrum which may lead to a lack in Fe, Si (BARTH), thus in case of submarine eruptions to the formation of siliceous iron ore (Lahn, Dill, RÖSLER). In sedimentary concentrates (Batolite, Laccolite, vein facies) this effect is marginal and not regional. c) The alkaline magmatic facies may be derived palingenetically from the orogenic compression, and within this the Atlantic and sedimentary concentrates are of a smaller compression state and may form in dehydrated zones; the Mediterranean, however, in that of a higher compression state. The principle of genetics may be described by way of irreversible thermodinamics and in this way the P. ESKOLA facii of metamorphites may genetically connected with the magmatic facii both in space and time. About these investigations being in course of action we shall report in some other paper. Literature: — 1. BENSON, W. N.: Spilitic lavas and radiolarian rocks in New South Wales (Geol. Mag., 10, 1913). — 2. BOWEN, N. L.: Genetic features of Alnóitic rocks at Isle Cadieux, Quebec (Am. Journ. of Sc., 3, 1922). — 3. BURRI, G. R.: Chemismus und provinzielle Verhältnisse der jungeruptiven Gesteine des Pazifischen Ozeans und seiner Umrandung (Schweiz. Min.-Pet. Mitt., No. 6, 1926.) — 4. BURRI, C. & NIGGLI, P. : Die jun gen Eruptivgesteine des Mediterranen Orogens. I — II (Schweizer Spiegel-Verlag, Zürich, 1945). — 5. Busz, K.: Heptorit, ein Hauyn — Monchiquit aus dem Siebengebirge am Rhein (N. Jb. Min. Petr. etc., 2, 1904). — 6. CHAYES, F.: Alkaline and carbonate intrusives near Bancroft, Ontario (Bull. Geol. Soc. Amer., 53, 1942). — 7. COTTA, B.: Eruptive Gesteine und Erzlagerstätten im Banal und Serbien (Berg- und Hüttenmann Zeitung, No. 14, 1864). — 8. GROSS, W., IDDINGS, J. & PIRSSON, L. & WASHINGTON, H.: A quantitative chemico-mincralogical classification of igneous rocks (Journ. of Geol. 10, 1902). — 9. COLEMAN, A. P.: A new analice rock from Lake Superior (Journ. of Geo!., 7, 1890). — 10. CSALAGOVITS, J. I. : Data to the alkaline magmatism of the Mecsek mountains. — Adatok a Mecsek-hegység alkáli magmatizmusához. (MTA. Geok. Konf. short report, 1959). — 11. CSALAGOVITS, J. I. : Thermodinamics of transvaporisation (Manuscript). — 12. CSALAGOVITS, J. I.: The chemical system of Trachidolerites, some questions of the genesis of Atlantic rocks viewed from the standpoint of transvaporisation (MTA. Geok. Konf. short report, 1959). — 13. DALY, R. A.: Origine of the alkaline rocks (Bull. Geol. Soc. Am., 21, 1910). — 14. DALY R. A.: The Geology of Ascension Island (Proc. Amer. Acad. Arts Sei, 00, 1925). — 15. DALY, R. A.: The Geology of St. Helena Island (Proc. Amer. Acad. Arts Sei, 62, 1927). — 16. DALY, R. A. & BARTH, T. F. W.: Dolerites associated with the Karroo System (S. Africa. Geol. Mag, 47, No. 789, 798, 1930). — 17. EAKLE, A. S.: A biotite—tinquaite dike from Manchester by-the-Sea, Essex Co. Mass. (Amer. Journ. Sei., 6, 1898). — 18. ERDMANNSDÖRFFER, O. H.: Über Vertreter der Essexit — Theralitreihe unter den diabasartigen der deutschen Mittelgebirge (Monatsber. Deutsch. Geol. Ges., 59, No. 2, 1907). —19. GLANGEUD, P.: Les régions vulcaniques du Pays de Dome (Bull, de la carte géol. de la France, No. 123, 1909). — 20. GOLDSCHMIDT, V. N.: Geologisch-petrographische Studien im Hochgebirge des südlichen Norwegens. Übersicht der Eruptivgesteine im Kaledonischen Gebirge zwischen Stavanger und Trondhjem (Skrifter Videnskap. Selsk. M. N. Kl. Kristiania, 75, 79, 1916). — 21. IDDINGS, J. P. : Igneous rocks (Vol. I. Composition texture and classification London , 1909, Vol. II, Description and occurence, New York —London, 1913). — 22. JENSEN, H. J.: The distribution, origin and relationships of alkaline rocks (Proc. Linnean Soc. N. S. Wales, 33, 1908). — 23. JOPLIN, G. A.: On the tectonic environment of basic Magma (Geol. Magazine, 1960, p. 362—368). — 24. JUHÁSZ, Á.: Pétrographie examination of palaeozoic Magmatites of the Balaton upland. — Balaton felvidéki paleozoós magmatitok kőzettani vizsgálata. (Föld. Közi., 1960, 90, 2, p. 157—171). — 25. KENNEDY, W. Q.: Trends of differentiation of basaltic magmas (Amer. Journ. of Sei. 5th, 25, No. 147, 1933). — 26. LACROIX, A. (2): Les syenites et ribeckites d'Alter Petroso Portugal, leurs formes mésocrates (lusitanites) et
