| Moquegua Basin | |
|---|---|
| Cuenca Moquegua | |
| Coordinates | 16°48′S70°48′W / 16.800°S 70.800°W | 
| Etymology | City of Moquegua, Peru | 
| Location | Western South America | 
| Country |  Peru | 
| State(s) | Department of Moquegua | 
| Cities | Moquegua | 
| Characteristics | |
| On/Offshore | Onshore | 
| Part of | Circum-Pacific forearc basins | 
| Hydrology | |
| Sea(s) | Eastern Pacific Ocean | 
| River(s) | Osmore River | 
| Geology | |
| Basin type | Forearc basin | 
| Orogeny | Andean | 
| Age | Cenozoic | 
Moquegua Basin is a sedimentary basin in southernmost Peru. Sedimentary rocks of the basin, including those of Moquegua Group, [1] crop out in the Central Depression makes up part of the sedimentary fill of the basin. [2] The basement of the basin is made of rocks older than the Cenozoic. [2]
Despite being close to the Pacific Ocean Moquegua Basin appear to have been unaffected by the Oligo-Miocene marine 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]