P. Alexandrov et al., Ionic microprobe dating of zircons from the Upper Gneiss Unit (South Limousin, Massif Central, France)., CR AC S IIA, 332(10), 2001, pp. 625-632
Citations number
36
Categorie Soggetti
Earth Sciences
Journal title
COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II FASCICULE A-SCIENCES DELA TERRE ET DES PLANETES
The Vergonzac leptynites in the Tulle anticline (South Limousin, West Massi
f Central) belong to the Upper Gneiss unit. The emplacement age of their pr
otolith was obtained by U-Pb ion-probe dating on selected zircons with CAME
CA IMS 1270. This age is 525 +/- 12 Ma, and is the same as the Mulatet orth
ogneiss and the Tulle Augen-gneiss, which belong to the Lower Gneiss unit.
This might imply that the protoliths of these two units were emplaced in th
e same geotectonic domain. (C) 2001 Academie des sciences / Editions scient
ifiques et medicales Elsevier SAS.