Titlebook: Intracontinental Fold Belts; Case Studies in the Henno Martin,Franz Wolfgang Eder Conference proceedings 1983 Springer-Verlag Berlin Heide

抱狗不敢前

Nappe Tectonics in the Southeastern Part of the Rheinisches Schiefergebirgeaphic and tectonic findings..The Gießen Greywacke, a turbidite sequence in the northeastern Lahn Syncline, rests unconformably on Lower through Upper Devonian rocks. Conodonts retrieved from carbonate-cemented greywackes, together with data from the literature, suggest that most (if not all) of the

食道

Flysch-Sedimentation: Its Relations to Tectonism in the European Variscidesre in every case directed outward from the ridge..Phenohercynian (northern external Zone): South Portugal, Southwest Fngland-, Pheinisches Schiefergebirge, Harz, with a possible continuation into Moravia (Č.S.S.R.). The source-area in Central Furope is the region of the Mid-German Crystalline Pise a

门闩

Migration of Folding and Metamorphism in the Rheinische Schiefergebirge Deduced from K-Ar and Rb-Sr shifting of flysch sedimentation..In order to get an idea of the time span which the “wave” of folding and metamorphism has needed to pass through the Rheinische Schiefergebirge, isotopic investigations by K-Ar and Rb-Sr methods were carried out. For these measurements the fine mineral fractions <2μ

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Experimental Study of Subfluence Tectonics in the Rheinische Schiefergebirgerelative to the mid-German Crystalline Rise and the boundary condition for isostatic movement following the crustal thickening are the main considerations in the present model experiments..In the model a syncline is formed as the major structure in the supracrust. The weak infracrust also has played

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GULLY

Intracrustal and Subcrustal Thrust-Tectonics at the Northern Margin of the Bohemian Massiflistic concept for the geotectonic developement of these regions..The origin of the Saxothuringian basin can be referred to an Upper Proterozoic to Ordovician rifting process. Metamorphosed sedimentary and basic igneous rocks found along the western margin of the Moldanubian Zone and in the Tepla-Pa

Anhydrous

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