Abstract
Four new SHRIMP U-Pb zircon ages older than 93 Ma from samples of the two uppermost formations accumulated in two different depocenters (Golfo de San Jorge and Cañadón Asfalto basins) of the Chubut Group in central Argentinean Patagonia, establish a pre-late Cenomanian-? early Turonian age for the group. It also confirms a coeval and comparable evolution of the two depocenters, where distal pyroclastic material was deposited together with fluvial and lacustrine facies.
Original language | English |
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Pages (from-to) | 67-74 |
Number of pages | 8 |
Journal | Journal of South American Earth Sciences |
Volume | 50 |
DOIs | |
Publication status | Published - Mar 2014 |