Intracontinental Fold Belts: Case Studies in the Variscan Belt of Europe and the Damara Belt in Namibia [Paperback]

Generalized Comparison of the Variscan with the Damara Orogen.- The Variscan Belt of Central Europe.- Palaeozoic Sedimentation in the Northern Branch of the Mid-European Variscides  Essay of an Interpretation.- Neritic Sedimentation of the Lower and Middle Devonian in the Rheinische Schiefergebirge East of the River Rhine.- Pelagic Carbonates in the Variscan Belt  Their Sedimentary and Tectonic Environments.- Devonian and Carboniferous Limestone-Turbidites of the Rheinisches Schiefergebirge and Their Tectonic Significance.- Depositional Models for the Carboniferous Flysch of the Eastern Rheinisches Schiefergebirge.- Flysch, Olistostromes and Nappes in the Harz Mountains.- The Mineral Composition of Rhenohercynian Flysch Sediments and Its Tectonic Significance.- The Sedimentary Development of the Western Rheinisches Schiefergebirge and the Ardennes (Germany/Belgium).- The Chemical Composition of Sedimentary Deposits in the Rhenohercynian Belt of Central Europe.- Chemical Composition and Genetic Relations of Meta-Volcanic Rocks from the Rhenohercynian Belt of Northwest Germany.- Mineral Composition of Pelitic Sediments in the Rhenohercynian Zone.- Nappe Tectonics in the Southeastern Part of the Rheinisches Schiefergebirge.- Flysch-Sedimentation: Its Relations to Tectonism in the European Variscides.- Migration of Folding and Metamorphism in the Rheinisches Schiefergebirge Deduced from K-Ar and Rb-Sr Age Determinations.- Experimental Study of Subfluence Tectonics in the Rheinische Schiefergebirge.- Regional Isostatic Model for Vertical Movements in the Shelf Area of the Rhenohercynian Geosyncline.- Intracrustal and Subcrustal Thrust-Tectonics at the Northern Margin of the Bohemian Massif.- The Crustal Structure of the Hercynian Mountain System  A Model forCrustal Thickening by Stacking.- Geodynamic Interpretation of the Mid-European Variscides.- The Damara Orogen.- Overview of the Geosynclinal, Structural and Metamorphic Development of the Intracontinental Branch l�