Despite being close to the Pacific Ocean Moquegua Basin appear to have been unaffected by the Oligo-Miocenemarine transgression that affected many other basins of western South America such as nearby Pisco Basin.[3] Concurrent with Andean uplift it is thought that the basin went from having a “balanced basin-fill” between Oligocene and Middle Miocene having a “overfilled basin-fill” from the Middle Miocene to the present.[1]
References
^ abAlván, Aldo; Ramírez, Katerine; von Eynatten, Hilmar; Dunkl, István; Jacay, Javier; Bertone, Gabriela (2017). "Evolución Geológica de las Cuencas de Antearco del Sur de Perú (Moquegua y Camaná-Mollendo): Proveniencia Sedimentaria y Análisis de Facies en Rocas Cenozoicas". Boletín de la Sociedad Geológica del Perú (in Spanish). 112: 053–077.