Orthogneisses in the deepest levels of the Variscan belt are not a Precambrian basement but Ordovician granites: tectonic consequences |
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Authors: | Maurice Mattauer |
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Affiliation: | Laboratoire « Dynamique de la lithosphère », UMR 5573 CNRS – université Montpellier-2, place Eugène-Bataillon, 34095 Montpellier cedex, France |
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