Browsing by Subject "Variszisch-herzynische Orogene {Geologie}"
Now showing items 1-4 of 4
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Fossil overpressures compartments? A case study from the Eifel area and some general aspects
; Bücker, Carsten; (11. Symposium "Tektonik, Struktur- und Kristallingeologie", 2006-03)
Fluid overpressures are well known from hydrocarbon exploration in many sedimentary basins. They can reach almost lithostatic values, and may cause the fracturing of rock. Fracturing allows the discharge of fluid overpressure, ... -
Lithospheric and upper mantle structure beneath the western Bohemian Massif obtained from teleseismic P and S receiver functions
(GFZ, Helmholtz-Zentrum[Bibliothek des Wissenschaftsparks Albert Einstein] [Vertrieb], [Potsdam], 2006) -
Structural contacts in subduction complexes and their tectonic significance: the Late Palaeozoic coastal accretionary wedge of central Chile
Richter, Peter P.; Ring, Uwe; Willner, Arne P.; (Journal of the Geological Society, 2007)
Understanding the contact between the very low-grade metagreywacke of the Eastern Series and high-pressure metamorphosed schist of the Western Series in the Late Palaeozoic accretionary wedge of central Chile is fundamental ... -
Structural contacts in the Late Paleozoic accretionary wedge of central Chile and their tectonic significance for the evolution of the accretionary complex
Richter, Peter P.; Ring, Uwe; Willner, Arne P.; (11. Symposium "Tektonik, Struktur- und Kristallingeologie", 2006-03)
The Chilean accretionary wedge is part of a Late Paleozoic subduction complex that developed during subduction of the Pacific plate underneath South America. The wedge is commonly subdivided into a structurally lower Western ...
