9786139868629 - Rhodope Morphotectonics and Seismic Hazard von Iliev, Rosen; Tzankov, Tzanko (8 Ergebnisse)

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Taschenbuch. Zustand: Neu. Rhodope Morphotectonics and Seismic Hazard | Rosen Iliev (u. a.) | Taschenbuch | 80 S. | Englisch | 2018 | LAP LAMBERT Academic Publishing | EAN 9786139868629 | Verantwortliche Person für die EU: preigu GmbH & Co. KG, Lengericher Landstr. 19, 49078 Osnabrück, mail[at]preigu[dot]de | Anbieter: preigu.

Taschenbuch. Zustand: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -The Rhodope Mountains ( = 23.8° - 26.3° E and phi = 40.8° - 42.0° N) is the largest mountain system in the eastern part of the Balkan Peninsula. The area of research is determined by the morphotectonics and structural-tectonics signs of the relief. As will be seen from the exposition and the appendixes to the text, the area in question is distinguished by ubiquitous morphostructural features of the same type that find a distinct expression in the topography. In this regard the main goal of this study is the morphotectonics analysis of regional conditions for the Late Quaternary endogenous risky processes, which is an attempt to build a general model of endogenous morphogenesis in the Rhodope Mountains. The study is based on prevailing today Plate tectonics model and also on geosynergy principle approach. Certain correlation studies have also been carried out on the prerequisites for the emergence of regional endogenous risk processes, expressed by the nature of the spread of earthquakes and the associated seismic hazard. 80 pp. Englisch.

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Zustand: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Autor/Autorin: Iliev RosenRosen Iliev is a Ph.D. in the field of Physical Geography. He has scientific interests in the areas of Geomorphology, Plate tectonics, Morphostructural analysis, (Geo)Fractal analysis, Seismic hazard, Geosynergy, Natural h.

Taschenbuch. Zustand: Neu. This item is printed on demand - Print on Demand Titel. Neuware -The Rhodope Mountains (¿ = 23.8° - 26.3° E and ¿ = 40.8° - 42.0° N) is the largest mountain system in the eastern part of the Balkan Peninsula. The area of research is determined by the morphotectonics and structural-tectonics signs of the relief. As will be seen from the exposition and the appendixes to the text, the area in question is distinguished by ubiquitous morphostructural features of the same type that find a distinct expression in the topography. In this regard the main goal of this study is the morphotectonics analysis of regional conditions for the Late Quaternary endogenous risky processes, which is an attempt to build a general model of endogenous morphogenesis in the Rhodope Mountains. The study is based on prevailing today Plate tectonics model and also on geosynergy principle approach. Certain correlation studies have also been carried out on the prerequisites for the emergence of regional endogenous risk processes, expressed by the nature of the spread of earthquakes and the associated seismic hazard.VDM Verlag, Dudweiler Landstraße 99, 66123 Saarbrücken 80 pp. Englisch.

Taschenbuch. Zustand: Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - The Rhodope Mountains ( = 23.8° - 26.3° E and phi = 40.8° - 42.0° N) is the largest mountain system in the eastern part of the Balkan Peninsula. The area of research is determined by the morphotectonics and structural-tectonics signs of the relief. As will be seen from the exposition and the appendixes to the text, the area in question is distinguished by ubiquitous morphostructural features of the same type that find a distinct expression in the topography. In this regard the main goal of this study is the morphotectonics analysis of regional conditions for the Late Quaternary endogenous risky processes, which is an attempt to build a general model of endogenous morphogenesis in the Rhodope Mountains. The study is based on prevailing today Plate tectonics model and also on geosynergy principle approach. Certain correlation studies have also been carried out on the prerequisites for the emergence of regional endogenous risk processes, expressed by the nature of the spread of earthquakes and the associated seismic hazard.