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In this study, we explore interrelationships between topography and tectonics in the central Iberian Peninsula.
This invariably implies that these lineaments might have resulted from plate movements and tectonics in the region.
A channel fill sequence in the upper catchment of the Khari river in the south of the Katrol Hill Fault (KHF) has been investigated to understand the role of climate and tectonics in the evolution of fluvial landforms.
However, the two Caucasus ranges are characterized by decidedly different tectonic regimes and rates of deformation that are subject to moderate (less than an order of magnitude) gradients in climate, and thus allow for a unique opportunity to isolate the effects of climate and tectonics in the evolution of topography within active orogens.
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Micropaleontological studies of the Late Pliocene to Early Pleistocene Japan Sea have been comprehensively reviewed, and the relationships between the major changes in the microfossil assemblages and both global climate and local tectonics in the Japanese Islands have been discussed.
The linear structures of tectonic origin offer valuable information concerning the seismic hazards and (neo) tectonics in the terrain (Macenzie 1978; Rastogi 2001).
Integrated stratigraphical and sedimentological research reported here focuses on palaeogeographical evolution, and particularly the response of the fluvio-deltaic systems to climatic and tectonic controls in the Late-Neogene sedimentary succession, in the eastern part of the Pannonian Basin.
Post- and pre-salt tectonics in the northern part of Sinai, the Nile Cone, and how they affect the structural framework and the seismic interpretation work in the study area are described.
The study of facies stacking patterns and sedimentary deformation structures in the Enugu Okigwe area of the Anambra Basin provides understanding of the nature and role of tectonics in the Campanian Maastrichtian sedimentation.
The sediment supply, northern continental slope system, paleo-geomorphic characteristics and tectonic setting in the Qiongdongnan Basin are considered as the controlling factors on the development and evolution of the Central Canyon System, each of them have different influences in the three segments.
The latter relate to major oceanographic and tectonic events in the region, including changing ocean circulation as a result of the closure of the Panama isthmus, and Caribbean plate dynamics that affected sea-floor and island topography.
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