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- W1595068901 abstract "La distribucion de mares y tierras durante el lapso Cretacico Superior-Oligoceno sugiere que, a finales del Cretacico, el rio Orinoco fluia hacia el noroeste. Durante el Oligoceno temprano, la direccion de su curso migro gradualmente en el sentido de las agujas del reloj y el Orinoco fluyo finalmente a traves del abra de Chivacoa hacia el norte, descargando sus aguas en el extremo oriental de la cuenca de Falcon. Solo finalizando el Oligoceno pudo el Orinoco irrumpir hacia el este, a traves de Ia silla formada por el alto de El Baul y el escudo de Guayana y desembocar en la cuenca de Venezuela oriental y mas tarde en el Atlantico. ABSTRACT The distribution of land and sea during late Cretaceous to Oligocene time suggests that at the close of the Cretaceous the Orinoco River flowed towards northwest. During the early Oligocene the trend of its course shifted gradually clockwise and the Orinoco flowed finally through the Chivacoa gap towards north and discharged into the easternmost Falcon Basin. Only late in the Oligocene could the Orinoco break through towards east the saddle between the El Baul Swell and the Guayana Shield and pour into the Eastern Venezuela Basin and later into the South Atlantic." @default.
- W1595068901 created "2016-06-24" @default.
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- W1595068901 date "2014-08-15" @default.
- W1595068901 modified "2023-09-23" @default.
- W1595068901 title "Notes on the shifting course of the ancient río Orinoco from late Cretaceous to Oligocene time." @default.
- W1595068901 hasPublicationYear "2014" @default.
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