TY  - JOUR
AU  - Maurice Mattauer
TI  - Orthogneisses in the deepest levels of the Variscan belt are not a Precambrian basement but Ordovician granites: tectonic consequences
JO  - Comptes Rendus. Géoscience
PY  - 2004
SP  - 487
EP  - 489
VL  - 336
IS  - 6
PB  - Elsevier
DO  - 10.1016/j.crte.2004.03.001
LA  - en
ID  - CRGEOS_2004__336_6_487_0
ER  -