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Neotectonics in Northern Portugal. A geomorphological approach in Abstracts of Papers and Posters. Vol. 1.
1989

Two types of platform plains - mobile and relatively stable are distinguished according to the rate of neotectonic geomorphic processes and position of endogenous sources of energy. Mobile areas are vast marginal parts of platforms up to hundreds
kilometers wide which are distinguished by elevated neotectonic activity induced from adjacent orogenes. The rate of neotectonic and geomorphic processes progressively increases towards mountains and nearly reaches values typical for the orogenous regions
1989

Neotectonism along the Atlantic passive continental margin : a review in Appalachian geomorphology.
1989

Three subzones of different age are distinguished within the zone of neotectonic deformations at the Southern Khibini on the basis of space photoes and geological-geomorphological data. The zone as a whole is associated with the large regional
lineament which has been reactivated at the neotectonic stage| it delimits the Imandra-Varzuga structural-facies zone. The zone's morphology clearly displays traces of paleoseismic deformations dated from the Late Pleistocene and Holocene. - (L'Ed.).
1989

of various mechanisms of neotectonic movements (block, fold movement etc.) for the relief-formation within both individual mountain regions and different types of geotecture. - (L'Ed.).
1989

Neotectonic structures of the Altai, Tien Shan und Dzungar Alatau have much in common, the mountain regions forming a single Central Asian belt. Its main structural elements are zones of linear deformations, large basins and the central Dzungarian
1989

This paper describes how mass movement is dissecting a relict alluvial fan at the margin of the Sele Valley graben. Rock mass structure and neotectonics are treated here, not as controls upon fan sedimentation, but as a fundamental cause
1989

Main stages of post-glacial development of the shelf topography in the East Siberian and Chukchi seas are considered. New data permit to trace the submerged coastlines (dated back to the last transgression) and to understand the neotectonic
1989

on the Barents and Kara shelves. The leading part of the neotectonics in the formation of the relief and correlate sediments is argued. The principal stages of relief formation and sedimentation through the Cenozoic are shown to correspond to certain phases
1989

of deformations of the initial - Pre-Eocene - planation surface permitted to construct a schematic map of amplitudes of neotectonic movements which formed principal features of the topography. The movements after the surface had been formed were mostly vertical
1989

the neotectonic and Pleistocene stages. The direction, rate and contrasts in the movements are assessed. Using instrumental data the geodynamics permit to trace alternating uplifts and subsidences as a reflection of the compression - tension mechanism during
1989

of contact between structures and blocks| sources of low order rivers are situated at neotectonic uplifts. Gullies formation is also typical for positive structures. An examination of fluvial erosion and debris transport directions permits to outline about 50
1989

place early during interglacial or warm phases, alluviation proceeded mostly during early glacial, full glacial and late glacial time. Erosion-alluviation alternation was mostly controlled by climate and in lesser degree by isostasy and neotectonics
1989

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