Diurnal asymmetry of radio wave absorption on anomalous winter days

au uu nu a¶rt;u a amma a nu¶rt; 1966–1981 naa, m ¶rt;, auu m m, u nu u ¶rt; uu n n¶rt;, ¶rt;num nu aa ¶rt; ¶rt;a n n¶rt;. m uu aa ¶rt;u u mu u.     

The relation between the magnitude derived from surface and from body waves for station průhonice

auam aum¶rt;, m u n¶rt; n a¶rt;u u nm a anu, umua a u mauu u 1964–1976 . ¶rt; aum¶rt; ma auau aum¶rt;, n¶rt; uu m .     

Temperature-time dependence of the electrical conductivity of garnets

aam mam uu mn¶rt;muaamuu n¶rt; u u nua ua —aam auumu m mnam (200–1000°, ₂ 10^–1 a). aa¶rt;u, m um na¶rt;a uu a n¶rt;u auumu mn¶rt;mu m mnam, u¶rt;m auumu ¶rt;a mn¶rt;mu mnam u n¶rt;m mu mnam uma.     

The IMF structure effects in vernal and autumnal midlatitude ionosphere

au a u naam u a nu¶rt; 1963–1973 . naam, m aum mun ma m mm nam aum n (II) na¶rt;am m u a uu ¶rt; u u,¶rt; ua ma u¶rt;, u u¶rt;a ma mn muna. mu u m ¶rt;u mam nm nmum n¶rt;auma amu m m mm II u a¶rt; ¶rt; n.     

A simple model of a building cumulus cloud

Summary A model of a building cumulus structure is described. The one-stage model published in[1] was used to describe ascent of two cloudy parcels that a cloud is supposed to be formed of. The other ascent is assumed to take place after the first cloud element sinks back as a result of evaporative cooling. The numerical results and their evaluation are given for various rates of mixing at the cloud top level of the first cloud volume.     

Time pattern of large earthquake sequences in Europe in 1976–1979

Summary The time development of three large sequences, Friuli 1976, Thessaloniki 1978 and Monte Negro-Albania 1979, was investigated by analysing the characteristics of the time distribution of magnitudes of the events, M(t), of average magnitudes, (t), and of the number of events, n(t), as well as the strain release curves and the magnitude-frequency relations, N(M). The existence of time gaps and of an anomalous decay of the numbers of shocks before major events, as well as the oscillation of ( const b^–1) may be considered as precursory phenomena. The clustering of events has been tested by the Poisson and negative binomial laws.Communication presented at the XVIIth General Assembly of the European Seismological Commission in Budapest, 21–29 August, 1980 under the title Properties of Seismic Regime and Recent Earthquake Sequences in Europe.     

A detailed study of the duality relation for the least squares adjustment in euclidean spaces

The Euclidean spaces with their inner products are used to describe methods of least squares adjustment as orthogonal projections on finite-dimensional subspaces. A unified Euclidean space approach to the least squares adjustment methods “observation equations” and “condition equations” is suggested. Hence not only the two adjustment solutions are treated from the view-point of Euclidean space theory in a unified frame but also the existing duality relation between the methods of “observation equations” and “condition equations” is discussed in full detail. Another purpose of this paper is to contribute to the development of some familiarity with Euclidean and Hilbert space concepts. We are convinced that Euclidean and Hilbert space techniques in least squares adjustment are elegant and powerful geodetic methods.     

Problems of the „Pannonian Median Massif“ and the plate tectonic concept. Contributions based on the distribution of Late Paleozoic — Early Mesozoic isopic zones

After a short historical review of conceptions about the Pannonian Median Massif or Tisia, the distribution of Middle-Upper Carboniferous and Lower Triassic-Liassic facies is briefly examined on the two sides of the Zagreb-Zemplin line dividing into two main segments the basement of the Carpathian basin. It shows on the one hand, that the Igal-Bükk zone (Igal-Bükk eugeosyncline ofWein, 1969), thought to establish a connection between the NW-Dinarides and the Dinaric-type Bükkium, is only a tectonic zone and could never have been a paleogeographical unit. On the other hand, the northern, marginal part of Tisia (Mecsek-Bihor crystalline belt and its sedimentary cover;Dank &Bodzay, 1971) exhibits a development and facies characteristic of the northern (northeastern) marginal complex of the Tethys. Also, facies-transitions from the foreland toward the open sea are always of N S direction. All autochthonous explanations must face the striking differences along the Zagreb-Zemplin line, which seem to exclude the possibility that the northern part of Tisia was a central, partly emerged crystalline ridge (no facies-transitions toward N!); it was rather part of the northern (northeastern) marginal complex of Tethys. Therefore allochthonous models suggesting largerscale horizontal movements give a much more plausible explanation. The style of Late Hercynian development and the distribution of Lower Triassic-Liassic facies zones suggest, that Tisia was part of the northern (northeastern) shelf of the Tethys until the end of the Liassic (in accordance with the opinion ofBleahu), then split off and was wedged in by horizontal movements between the NW-Dinarides and the Dinaric-type Bükkium by the end of the Jurassic — beginning of the Cretaceous.

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Zusammenfassung Nach einem kurzgefaßten historischen Überblick zur Deutung des Pannonischen Massivs oder Tisia wird die Verteilung der Fazies von Mittel- und Oberkarbon sowie Untertrias bis Lias auf den beiden Seiten der Zagreb-Zemplin-Linie — welche den Untergrund des Karpatenbeckens in zwei Abschnitte zerteilt — kurz untersucht. Sie zeigt einerseits, daß die Igal-Bükk-Zone (die Igal-Bükk Eugeosynklinal vonWein, 1969)-welche eine Verbindung zwischen den NW Dinariden und dem dinarisch-typischen Bükkium darstellen soll — nur eine tektonische Zone ist, hingegen nie eine paleogeographische Einheit gewesen sein kann.Der nördliche, äußerste Teil des Tisia (Mecsek-Bihor kristalliner Gürtel und seine sedimentäre Decke;Dank u.Bodzay, 1971) weist eine Ausbildung und Fazies auf, welche für den nördlichen (nordöstlichen) marginalen Komplex der Tethys typisch ist. Auch Faziesübergänge vom Vorland in der Richtung der offenen See sind immer N S gerichtet. Alle Erklärungen, die eine autochthone Lage der Zonen entlang der Zagreb-Zemplin-Linie mit einbeziehen, müssen mit der Tatsache fertig werden, daß der nördliche Teil der Tisia einen zentralen Teil eines teilweise emporgehobenen Kristallinrückens darstellt (kein Faziesübergang nach Norden). Sie war eher Teil der nördlichen (nordöstlichen) marginalen Serie der Tethys. Daher erscheinen allochthone Modelle, welche horizontale Bewegungen in größerem Maßstabe andeuten, eher glaubwürdig zu sein. Der Stil der spätherzynischen Entwicklung und die Verteilung der Fazieszonen von Untertrias bis Lias deuten an, daß der Tisia Teil der nördlichen (nordöstliche) Shelf der Tethys bis Ende Lias war (übereinstimmend mit der Meinung vonBleahu 1976); dann spaltete er sich ab und keilte sich mit horizontalen Bewegungen zwischen den NW Dinariden und dem Bükkium dinarischen Types ein; dies könnte Ende Jura-Anfang Kreide stattgefunden haben.

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Résumé Après une brève revue historique des conceptions sur la »Masse médiane pannonienne« ou la »Tisia«, on examine brièvement la distribution des facies du Carbonifère moyen-supérieur et du Trias-Lias aux deux cotés de la ligne de Zagreb-Zemplin divisant le soubassement du Bassin Carpathique en deux ségments principaux.Ce qui est démontré, c'est d'une part que la zone Igal-Bükk (le »géosynclinal Igal-Bükk«, Wein, 1969), considérée comme l'établissement d'une communication entre les Dinarides du NW et le Bükkium de type dinarique, ne représente qu'une zone tectonique, mais qu'elle ne peut jamais être une unité paléogéographique. D'autre part la partie septentrionale, marginale de la »Tisia« (la ceinture crystalline de» Mecsek-Bihor« et sa couverture sédimentaire; Dank-Bodzay, 1971) présente un développement et un faciès caractéristique du complexe marginal septentrional (nordoriental) de la Téthys. Les transitions de faciès de l'avant-pays vers la mer ouverte sont également de direction N-S. Toutes les explications autochtonistes doivent faire face aux différences accentuées le long de la ligne Zagreb-Zemplin, ce qui semble exclure la possibilité que le Nord de la »Tisia« ait été une dorsale cristalline centrale, émergée (aucune transition de faciès vers le N!); elle a fait plutôt partie du complexe marginal du N (NE) de la Téthys. C'est pourquoi les modèles allochtonistes suggérant des mouvements horizontaux plus vastes donnent une explication plus plausible. Le style du développement éohercynien et la distribution des zones faciales du Trias inférieur-Lias suggèrent que la »Tisia« a fait partie du shelf septentrional (nordoriental) de la Téthys jusqu'à la fin du Lias (en accord complet avec l'opinion de Bleahu, 1976) et qu'ensuite elle s'était décollée et coinné par des mouvements horizontaux entre les Dinarides du NW et le Bükkium de type dinarique vers la fin du Jurassique et le début du Crétacé.

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Because of shortage of place, only some of the most important non-Hungarian literature and the latest Hungarian works concerned with this region are listed up here: for a more detailed list of reference the reader is referred to the papers ofBalogh (1972) andKovács (1980).     

Dissolution of secondary copper sulphides using complex-forming agents (EDTA,EDA). Part I: Covellite dissolution in EDTA and EDA

Problems of dissolution of the so-called secondary copper sulphides are very important for dynamic as well as percolation leaching of ores. This paper deals with dissolution kinetics of sulphides in an alkaline medium, using complex-forming agents in connection with possibility to leach basic, partially oxidized ores. Natural minerals and their polydispersions were investigated and the so-called geometrical model was used for evaluation. Basic dependences of the dissolution rate on the reagent concentration and pH value of the leaching solution were found and an attempt at their mathematical expression and physical interpretation was made. The first part of this work refers to the systems of covellite-ethylene diamine tetra-acetic acid (EDTA) and covellite-ethylene diamine (EDA). The established dependences are not only of theoretical but also of practical importance.