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Orogenesis and morphogenesis of outer Carpathians and plate tectonics
The orogenesis of the Outer Carpathians seems to be a result of the subduction of the oceanic part of Euroasian plate. The beginning of the subduction in the flysch basin seems to be in the Eocene more precisely at anomaly /53m.l. At this time
, and then compressional deformations migrated outwards across the basin. Those processes were accompanied by Carpathian orogenesis. Compressional deformations continued in subaerally conditions during the last phase. The upper limit of the orogenesis migrated outwards
across the Carpathians. This agress with the diachronous scratching off deposits from a subducted plate. The orogenesis in the Carpathians occuried interruptedly and so-called orogenic phases alternated with periods of calm. But the results of an analysis
of joints in the Nowy Sacz Basin seem to attest that, this region was under compression from at least the Eocene up to the Lower Bedanian Later, this region was exclusively under tension. The result of that was the Carpathian orogenesis. (d'après l'A.).

Orogenèse et dislocations quaternaires du versant tyrrhénien des Abruzzes (Italie centrale). (Quaternary orogenesis and displacements on the Tyrrhenian side in the Abruzzi (Central Italy))

Drainage on the north and west flanks of the Miocene Lyttelton Volcano does not have the expected radial and consequent pattern. It is proposed that the term anteconsequent, previously used in the context of orogenesis and erosion, should

intermountain plain. Morphology of the tectonic relief suggests that lithospheric blocks within the mountain belt underwent strong horizontal crushing and longitudinal flow. Arch-block orogenesis (of Gobian type) prevails, mountains growing at the expense

The land-ocean ratio, periodical alternation of the epochs of orogenesis and peneplanation, time-space changes of solar influx determined the periodical changes of the global hydrological cycles with development of the continental glaciations

Alpes ; Esquisto ; Estratigrafía ; Geología regional ; Italia ; Litología ; Orogénesis ; Roca metamórfica

Out of the possible models of a mantle-related granite genesis in the Erzgebirge Mts. a diapirism model is favoured according to which with the beginning of Variscan orogenesis a mantle diapir became active in Europe. From the mantle uparching

The development of the recent drainage system in the Rhenish Mountains started during Late Oligocene by the Alpine orogenesis. Still the Early Tertiary time the drainage on the strongly weathered Variscans took place by unlarged flushing areas

Cenozoíco ; Descolgamiento ; Falla ; Geología regional ; Impacto ; Neogeno ; Orogénesis ; Tectónica ; Tensión de cizallamiento

Cuaternario ; Estratigrafía ; Geología regional ; Neogeno ; Orogénesis ; Sísmica marina ; Tectónica

Cuenca sedimentaria ; Estratigrafía ; Geología regional ; Modelo ; Neogeno ; Orogénesis ; Sísmica marina ; Tectónica

Corriente de agua ; Evolución del valle ; Geomorfología ; Hungría ; Orogénesis ; Valle

Cabalgado tectónico ; Geología regional ; Geomorfología estructural ; Italia ; Mapa geológico ; Orogénesis ; Sicilia ; Tectónica

Cabalgado tectónico ; Geología regional ; Geomorfología estructural ; Italia ; Orogénesis ; Toscana

of naps indicate an enormous short-cutting of the earth's crust under the Caledonian orogenesis. At the same time, the Pre-Cambrium nap-zones and the underlying layers also indicate similar short-cuttings and nappings during earlier orogonesis

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