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Title of Journal: Int J Earth Sci Geol Rundsch

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Abbravation: International Journal of Earth Sciences

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Springer-Verlag

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DOI

10.1016/0003-9861(86)90754-x

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1437-3262

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Reply to W Franke on W Dörr and G Zulauf elevat

Authors: W Dörr G Zulauf
Publish Date: 2012/04/03
Volume: 101, Issue: 7, Pages: 2035-2041
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Abstract

In his comments on our paper about Variscan elevator tectonics W Franke this issue presents several reasons which—according to his view—would not be compatible with overthickened crust in the TepláBarrandian unit during Upper Devonian/Lower Carboniferous continent/continent collision In the following paragraphs we will show that 1 most points addressed by W Franke are not relevant for our model of elevator tectonics 2 correlations made by W Franke between various crustal blocks of the Bohemian Massif are not consistent with data and 3 the models presented by W Franke are based on assumptions but ignore a complete set of robust dataW Franke is pointing out that the Barrandian Paleozoic rocks underwent only minor shortening less than 20  There would be no evidence for major thrust stacking under the Paleozoic cover and the diagenetic grade of the Devonian rocks would preclude the once former existence of higher structural units These observations would


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