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  • Neotectonic movements in the Sperkhios River basin, Central Greece in Neotectonics and morphotectonics.
  • Caves as indicators of neotectonics in Sweden in Neotectonics and morphotectonics.
  • Caves indicating neotectonic activity in Sweden
  • Neotectonics of the Polish Carpathians: facts and doubts
  • The influence of neotectonics upon valley floor development: a case study from the Wieprz Valley, Lublin Upland
  • Neotectonics in the Province of Blekinge
  • In this paper the parameters of neotectonic movements regime are considered. As the result the zoning of the Azerbaijan territory on neotectonic intensity is given.
  • Neotectonics in Northern Portugal. A geomorphological approach in Abstracts of Papers and Posters. Vol. 1.
  • Neotectonic movements of the polish West Carpathians
  • 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
  • A new method is introduced to classify and map regions by the earth-crust types and recent endogenous regimes. Areas of certain regimes when compared with neotectonic structure and topography manifest a great variety of the correlation. The author
  • concludes that the same neotectonic structures and similar types of topography (both positive and negative) may belong to areas of different endogenous regimes (both constructive and destructive). Some regions are indicated where neotectonic structures
  • Total amplitudes of neotectonic movements are usually calculated without taking into consideration the Cenozoic lowering of the World Ocean level, which results in grave errors in views on tectonics and geomorphology, as the value of the lowering
  • is about few hundreds meters (no matter what lower limit of the Cenozoic stage is assumed). The A. introduced a correction which he used for neotectonic mapping of the Siberian Platform. Using the correction, the vast area of neotectonic downwarping (about
  • A Balaton kornyéki neotektonika. (Neotectonics in the Lake Balaton region)
  • Verhu neotektonskata aktivizacija na razlomnite strukturi v Belgarija On the neotectonic activation of fault structures in Bulgaria
  • During the Plio-Pleistocène, the Peloponnesus is a very unstable peninsula. The fault-scarps (tectonic or partly rejuvenated show various interactions between neotectonic throws and climates, which were able to shape different slopes, largely
  • concave between Villafranchian and Riss, partly rectilinear during the cold Riss and Würm in the limestones. The lowest marine terrasse and the ionian shoreline put the question of the interactions between the Neotectonics and the glacio-eustatic
  • The eastern Caucasus is an example of correlations between morphostructure caracterized by the importance of soft rocks and neotectonics, the peculiar role of the Caspian base level, climatic changes and present day semiarid prevailing conditions
  • . The pliopleistocene stratigraphy and tectonic are pointed out together with the resulting landforms, the drainage patterns, the marine and continental terraces. The problems of climatic inherited forms, and their explanation by climatic changes or neotectonics
  • Indications of neotectonic feature in Denmark
  • 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.).
  • Within the limits of Byelorussia neotectonic processes controlled the pattern of the drainage net belonging both to the Black and Baltic sea drainage basins to a considerable degree. Differentiated neotectonic movements up to 150 to 170 meter range
  • Upper Pliocene-Pleistocene uplift rates as indicators of neotectonic pattern: an example from southern Calabria (Italy)