|Series||Proceedings of the Israel Academy of Sciences and Humanities, Section of Sciences, no. 9, Proceedings (Aḳademyah ha-leʼumit ha-Yiśreʼelit le-madaʻim. Ḥaṭivah le-madaʻe-ha-ṭevaʻ) ;, no. 9.|
|LC Classifications||QE606.5.E85 P5213|
|The Physical Object|
|Number of Pages||34|
|LC Control Number||75309068|
Crustal Structure of the Rhinegraben area. In: S. Mueller (Editor), The Structure of the Earth's Crust, based on Seismic Data, Tectonophysics 20 (1–4): – Numerous geological and geophysical investigations within the past decades have shown that the Rhinegraben is the most pronounced segment of an extended continental rift system in by: Two of the most important segments of the west European Rift, the Rhinegraben and the Massif Central grabens, show in plan and in cross section a very different crustal structure. The Rhinegraben. Abstract. The Rhinegraben is one of the best studied rift structures in the world. In the past 20 years, it has been the site of many seismic refraction studies. However, most of the profiles have only been interpreted using 1-D methods. In this paper a combined 2-D and 1-D analysis of the only reversed profile within the graben proper is by: Crustal Structure of the Rhinegraben area. In: S. Mueller (Editor), The Structure of the Earth 's Crust, based on Seismic Data, Tectonophysics 20 (): Numerous geological and geophysical investigations within the past decades have shown that the Rhinegraben is the most pronounced segment of an extended continental rift system in Europe. The structure of the upper and .
Tectonophysics, 73() 79 Eisevier Scientific Publishing Company, Amsterdam Printed in the Netherlands Crust and Mantle Structure THE CONTINENTAL RIFT SYSTEM OF THE RHINEGRABEN - STRUCTURE, PHYSICAL PROPERTIES AND DYNAMICAL PROCESSES * K. FUCHS, K.P. BONJER and C. PRODEHL Geophysikalisches Institut, University o f Karlsruhe, . The curves and the map contour lines of Fig. 1 summarize the main data that we have used. THE NORTHERN RHINEGRABEN The Rhine valley, approximately 40+5 km wide, is bounded by two master normal fault zones (Fig. ID). The structure and evolution of the Rhinegraben differ strikingly from north to south. Asthenosphere Structure and Anisotropy Beneath Rifts Adolphe Nicolas Crustal Evolution of the Rhinegraben Area: Exploring the Lower Crust in the Rhinegraben Rift by Unified Geophysical Experiments Karl Fuchs, K.-P. Bonjer, D. Gajewski, E. Luschen, c. Prodehl. 1 Crustal Structure of Central and Southeastern Europe by Data of Explosion Seismology. 2 Structure of the Earth's Crust on the Territory of the U.S.S.R. 3 Seismic Studies of Low-Velocity Layers and Horizontal Inhomogeneities Within the Crust and Upper Mantle on the Territory of the U.S.S.R.
The book focuses on the formation, behavior, and mechanisms of grabens. The selection first offers information on crustal doming and the mechanism of continental rifting, mechanisms of continental riftogenesis, and thermal regimes, mantle diapirs, and crustal stresses of continental rifts. J. Ansorge, D. Emter, K. Fuchs, J.P. Lauer, St. Mueller and E. Peterschmitt, Structure of the Crust and Upper Mantle in the Rift System around the Rhinegraben, in: Graben Problems, ed. by J.H. lilies and St. Mueller, Schweizerbart-Verlag, Stuttgart, Google Scholar. 2. Abstract. Detailed features of the crustal structure beneath the Black Forest basement complex (in southwestern Germany), the adjacent Jura mountains and Molasse basin (in northern Switzerland) combined with the eastern and southern geotraverses across the Swiss Alps have recently been surveyed by various geophysical methods. The group became known as the CREST working group, an acronym of Continental Rifts: Evolution, Structure and Tectonics, which not surprisingly became the title of this ental Rifts: Evolution, Structure, Tectonics presents an overview of the present state of understanding and knowledge of the processes of continental rifting from a.