Genesis of deformation structures affecting Plio-Pleistocene sediments in the western Portuguese mainland (West Iberia). Implication on the regional neotectonics
of the outcropping structures. The neotectonic activity is therefore reconsidered from the interpretation of the triggering mechanisms responsible for the observed deformation.
structures of the Sicilian Chain. This neotectonic system may be related to a W-E trending simple shear system, which controls the Tyrrhenian Basin development. - (NF)
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.
Investigations into interrelationships between geomorphology, neotectonics and seismicity in the Danube Plain and in the northern part of the Danube-Tisza Interfluve bear importance due to the socio-economic significance of these landscapes
. The results have been represented in thematic maps, where landscape boundaries based on genetic notions coincided with neotectonic fault lines in several places. In order to make geomorphological and tectonic models correct the geological sediments of the high
This paper discusses the morphological and geological evidence for Pleistocene neotectonic faulting and uplift in the northeastern part of the Sowie Mountains where the Sudetic Marginal Fault has its maximum deplacement and uplift rates. Although
The purpose of this paper is to describe and interpret neotectonic structures in the famous travertines at Pamukkale. Three morphological varieties of travertine mass are of structural significance: 1) range-front travertines cementing alluvial -fan