U-PB ZIRCON GEOCHRONOLOGY OF BRASILIANO G RANITOIDS FROM THE SERIDO OROGENIC BELT (BORBOREMA PROVINCE, NE BRAZIL)

Citation
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
Citations number
16
Categorie Soggetti
Multidisciplinary Sciences
ISSN journal
07644450
Volume
318
Issue
11
Year of publication
1994
Part
2
Pages
1505 - 1511
Database
ISI
SICI code
0764-4450(1994)318:11<1505:UZGOBG>2.0.ZU;2-T
Abstract
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.