1887

Abstract

In the Late Carboniferous (Namurian to Westphalian) the Variscan Foreland Basin of Central and Western Europe was formed north of the Variscan deformation front and extended 800 km parallel to the deformation front (Figure 1).

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/content/papers/10.3997/2214-4609.201408528
1998-06-08
2021-09-20
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