Evmilliok emlékei. Magyarorszag foldtorténete és asvanyi kincsei.. (Memories from millions of years. Geological evolution and mineral resources of Hungary)
The first part is a review for the major stages of geological evolution: the second is an attempt to explain this evolution on the basis of plate tectonics| the third is a summary of the major mineral resources and the fourth is a geological guide
The A. gives a review of oceanic areas of the world, which obtain increasing importance concerning in the development of geological sciences with regard to the basic geological research as well as to the applied geological research, especially
Sea-level change and water-level movements in The Netherlands during the Holocene. A contribution to Project 61 of the International Geological Correlation Programme
The distributions and affinities of the macrolepidopteran taxa known from south-eastern Polynesia are investigated and contrasted with various geological hypotheses for the origin of the islands. A colonialist interpretation, long distance dispersal
Results of an inventory of the largest deposits as well as the small occurrences of the district undertaken by the Geological Survey of Belgium. A model of the mechanisms of ore concentration and guides for the prospection are proposed. (LW).
The article is a short review on the Pre-Quaternary geological history of the The Hague area. Hydrocarbons, geothermal energy (plans) and groundwater exploitation are covered. (AIS).
is based on gravity, magnetic and geological data, and confirms the recently published geological schemes of this area thus amphasizing the importance of geophysical region division. Results of deep seismic soundings in the same area are discussed
Based on selected investigations, carried out in sulphate karst, ways to quantitive engeneering-geological results are pointed out. Such investigations always go back to comprehensive geological survey combined with geodetic work. Findings of other
Current methods in biogeography are briefly reviewed and definitions of dispersal discussed. The need for countenancing the possibilities of operation of both the vicariance and dispersal modes is stressed, and for taking into account geological