A Pannoniai-medence morfogenetikaja. (The morphogenetics of the PannonianBasin)
Bassin Pannonien ; Carte géomorphologique ; Europe ; Europe de l'Est ; Géographie physique ; Géomorphogenèse ; Géomorphologie structurale ; Hongrie ; Roumanie ; Tchécoslovaquie ; Tectonique ; Yougoslavie
The models for the origin of the PannonianBasin and the geomorphic history of its highland, hilly and plain morphostructures are outlined on the data basis of borehole analyses, correlation of geomorphological surfaces and geomorphological mapping
On understanding the range and stratigraphic position of the Pannonian in Problems of the Neogene and Quaternary in the Carpathian Basin.
Based on a joint analysis of molluscs, ostracods and mammals as well as available geological and paleogeographical information, an attempt was made to correlate the Pannonian sediments with those of Eastern and Mediterranean. DLO).
Pliocene and Pleistocene formations dominate in the PannonianBasin. The evolutionary history of relief is reconstructed with the aid of geomorphological surfaces (i.e. fluvial terraces, travertine levels, raised beaches) and faunal successions
The change from limnic to terrestrial sedimentation is regarded as a marker of the N/Q boundary in the Carpathian basin. It is roughly synchronous with the Matuyama-Gauss paleomagnetic reversal (million years). The boundary is easy to trace
in mountains, but more difficult to define in basins where oscillations of water level took place. DLO).
The crystalline complex of the Sopron Mts. at the eastern end of the Austroalpine nappe system and on the western rim of the PannonianBasin is a key area to investigate the relationship of orogenic and extensional-rift structures that led
to the formation of the PannonianBasin. The AA. focused primarily on the brittle and ductile deformations in 3 selected gneiss outcrops (Nádormagalast, Harka Hill, Kö Hill). Beyond providing evidence for the possible rotation and tilting of the different blocks
Discrimination of fluvial, eolian and neotectonic features in a low hilly landscape : a DEM-based morphotectonic analysis in the Central PannonianBasin, Hungary
Aeolian features ; Digital elevation model ; Drainage network ; Fluvial erosion ; Geomorphology ; Hungary ; Morphometry ; Neotectonics ; PannonianBasin ; Quaternary ; Wind erosion
The Gödöllő Hills, a low-relief terrain within the Central PannonianBasin in Hungary, is characterised by moderate tectonic deformation rates. Although typical tectonic landforms are not clearly recognisable in the study area, this paper succeeded
The Neogene red clays of the Carpathian basin in Problems of the Neogene and Quaternary in the Carpathian Basin.
Opinions differ as to whether the true red clays mostly deposited on Upper Pannonian lacustrine sediments are dated as Pliocene or early Quaternary. Biostratigraphic and lithostratigraphic data show that these non-rewashed residual deposits of red
Prinz, the geographer also contributed to geology by elaborating the Tisia theory, i.e. the origin of the Pannonianbasin due to the subsidence of a rigid rock mass, which caused the orogeneses encircling the mass. The reconciliation of the model
Bassin Pannonien ; Europe ; Géographie physique ; Tectonique de plaques ; Tectonique globale ; Tisia
A rigid Hercynian massif controlling the structure of the Carpathians and Dinarides below the Neogene sedimentary cover of the PannonianBasins named Tisia was supposed before the beginning of the systematic investigation of this area by deep
isostatically due to the changes in density of the lithosphere and to the subsidence of the thinned crust, producing the PannonianBasins. Finally basaltic partial melt products of the mantled arch heated gradually by the volatile emanations extrude, too
Macromorphologically, the study area in Pannonian Croatia is basically a mountain-and-basin region. Geologically, it is on the W border of the PannonianBasin, in contact with Forealpian structures. Special importance is rendered to tectonic
This article establishes whether Slovenia’s landscape diversity and its position at the intersection of four major European geographical units (the Alps, the Mediterranean, the PannonianBasin, and the Dinaric Alps) is also reflected in non
features of the rock samples the structural situation within the PannonianBasin as well as certain geochemical peculiarities on paleogeomorphological relations were also taken into consideration. (CK).
concepts, which stipulate that a large regional planation surface of Pannonian age developed in the whole Western Carpathians. The data indicate : a dynamic basin setting with an active accretionary process in a subduction zone; accretionary processes
The apatite fission track and apatite (U-Th)/He data measured on teschenite intrusions show that planation surfaces in the study area formed in post-Pannonian time and are therfore younger than traditionally believed. This contradicts the classical
On late Miocene-early Pliocene desert climate in the Carpathian Basin
Until recently only geomorphological features and mammal fossils had been known as evidence to the long-debated dry-warm semidesert or hot desert climate in the Carpathian basin following the filling up of the Pannonian Lake. A comparison of samples
A valodi voros agyag geomorfologiai helyzete és foldtani kora a Karpat-medencében (Situation géomorphologique et âge géologique de l'argile rouge authentique dans le Bassin Carpathique)
The true red clay is disclosed between 800-1 000 m depths in the Koros basin. The formation took place during the Upper Pannonian and subsequently during pedimentation. - (DLO)
The economic geological importance of the lignite at the foreland of the Northern Hungarian Uplands in Problems of the Neogene and Quaternary in the Carpathian Basin.
The defined productive area is economically the most valuable portion occupied in the Upper Miocene by the Pannonian inland lake, where 81.6 per cent of the country's economically recoverable lignite reserves are concentrated. The establishment
Bassin Pannonien ; Danube-Tisza ; Evolution du relief ; Géographie de l'Europe ; Géomorphogenèse ; Hongrie ; Hydrogéologie
The basic geological boreholes presented in this paper fall into the framework of a complex and detailed research program commenced in 1964. These boreholes disclose the entire Quaternary and Upper Pliocene and part of the Upper Pannonian