Orogenic wedge growth during collision — constraints on mechanics of a fossil wedge from its kinematic record (Rhenohercynian FTB, Central Europe)

Author:

Plesch A.,Oncken O.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference89 articles.

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2. Thickness of the Hercynian Ardenne sediment wedge restudied: implications for balancing of deep structural cross-sections;Adams;Aardk. Mededel.,1997

3. Ahrendt, H., Clauer, N., Hunziker, J.C., Weber, K., 1983. Migration of folding and metamorphism in the Rheinisches Schiefergebirge deduced from K–Ar and Rb–Sr age determinations. In: Martin, H., Eder, F.W. (Eds.), Intracontinental Fold Belts. Case Studies in the Variscan Belt of Europe and the Damara Belt in Namibia, Springer, Berlin, pp. 323–338.

4. Anderle, H.-J., Massonne, H.-J., Meisl, S., Oncken, O., Weber, K., 1990. Southern Taunus Mountains. In: Field Guide Mid German Crystalline Rise & Rheinisches Schiefergebirge. Int. Conf. Paleozoic Orogens in Central Europe, Göttingen–Gießen, pp. 125–148.

5. The concealed crystalline basement in Belgium and the `Brabantia' microplate concept: constraints from the Caledonian magmatic and sedimentary rocks;André;Ann. Soc. Géol. Belg.,1991

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