CICTERRA   20351
CENTRO DE INVESTIGACIONES EN CIENCIAS DE LA TIERRA
Unidad Ejecutora - UE
congresos y reuniones científicas
Título:
U-PB DETRITAL AGES ON TUFFACEOUS AND SANDSTONE LEVELS FROM A NEOGENE THICK FORELAND BASIN OF THE CENTRAL ANDES OF ARGENTINA.
Autor/es:
COLLO, GILDA; DAVILA, FEDERICO; EZPELETA, MIGUEL; TEIXEIRA, WILSON
Reunión:
Congreso; II Congresso de Geología dos países de Lingua Portuguesa; 2014
Resumen:
Six tuffaceous and sandstone levels from an Andean (Mio-Pliocene) synorogenic succession were
analyzed using the U-Pb LA-ICP-MS method on zircons, in order to constrain maximum
depositional ages and to define the basin provenance and likely connections
with the volcanic history of the South-Central Andes. The detrital ages of the
different samples were rather similar, ranging from ~2007 to ~5 Ma
(Paleoproterozoic to Cenozoic). The pool of ages suggests reworking and high
detrital contamination of the volcaniclastic levels. The main detrital
populations have age mode at 460 and 480Ma (Ordovician) and three main Andean volcanic
episodes at ~5, 13 and 21Ma were identified. From these new data sets, a
sedimentation rate of ~0.7mm/yr would characterize the basin fill between ~13
and 5 Ma.