J. Leterrier et al., U-PB ZIRCON GEOCHRONOLOGY OF BRASILIANO G RANITOIDS FROM THE SERIDO OROGENIC BELT (BORBOREMA PROVINCE, NE BRAZIL), Comptes rendus de l'Academie des sciences. Serie 2, Mecanique, physique, chimie, sciences de l'univers, sciences de la terre, 318(11), 1994, pp. 1505-1511
Diorites previously attributed to an early stage of the ''brasiliano''
plutonic evolution of the Serido belt yielded U-Pb zircon age of 579
+/- 7 Ma. The age of associated granites is slightly younger although
a synchronous emplacement of granites and diorites is suggested by fie
ld relationships. Such an age difference may result from difficulties
to distinguish 'crystallization age' from 'emplacement age'', which is
still to be determined precisely.