Caballos Formation should not be confused with Caballos Novaculite.
| Caballos Formation | |
| Period: | Albian |
| Age: | Aptian-Albian ~ |
| Type: | Geological formation |
| Prilithology: | Sandstone, shale, siltstone |
| Otherlithology: | Limestone, coal |
| Underlies: | Hondita Formation |
| Overlies: | Yaví & Saldaña Formations |
| Thickness: | up to 411m (1,348feet) |
| Map: | Blakey 105Ma - COL.jpg |
| Coordinates: | 3.8219°N -75.3562°W |
| Region: | Caquetá, Huila, Putumayo & Tolima Departments |
| Extent: | VSM & Caguán-Putumayo Basin Central & Eastern Ranges, Andes |
| Namedfor: | Cerro Caballos |
| Namedby: | Corrigan |
| Year Ts: | 1967 |
| Location Ts: | Olaya Herrera |
| Coordinates Ts: | 3.8219°N -75.3562°W |
| Paleocoordinates Ts: | -2.9°N -47.4°W |
| Region Ts: | Tolima |
| Thickness Ts: | 411m (1,348feet) |
The Caballos Formation (Spanish; Castilian: Formación Caballos, KI) is a geological formation of the Upper Magdalena Valley (VSM), Caguán-Putumayo Basin, Central and Eastern Ranges of the Colombian Andes. The sandstone and shale formation dates to the Middle Cretaceous period; Aptian to Albian epochs and has a maximum thickness of 411m (1,348feet).
The formation was defined and named in 1967 by Corrigan after Cerro Caballos, to the west of Olaya Herrera, Tolima.[1]
The Caballos Formation has a maximum thickness of 411m (1,348feet) in the Quebrada Bambucá and is characterized by a lower sequence of fine to coarse sandstones, of lithic arenite, quartz arenite and feldspar arenite composition, a middle section of fossiliferous black shales and siltstones, intercalated by micritic limestones and coals and very fine sandstones. The upper part of the formation contains conglomerates and glauconitic sandstones.[1]
The Caballos Formation in some parts concordantly overlies the Yaví Formation and in other parts rests unconformably on the Saldaña Formation and Ibagué Batholith.[2] The formation is overlain by the Hondita Formation. The age has been estimated to be Aptian to Albian. Stratigraphically, the formation is time equivalent with the Une, Aguardiente, Simijaca, El Peñón, Capotes, Tablazo, Tibú-Mercedes and Pacho Formations.[3] The formation has been deposited in a fluvial to estuarine and shallow marine environment.[4]
The Caballos Formation is a source, reservoir and seal rock in the Upper Magdalena Valley,[5] [6] and a source and reservoir rock in the Caguán-Putumayo Basin.[7] [8] The Orito and Moqueta Fields of the latter basin produce from Caballos reservoirs.
The formation has provided fossils of Heminautilus etheringtoni,[9] Araucarites sp., Brachyphyllum sp., Cladophlebis sp., and Weichselia sp.,[10] as well as many types of pollen.[11]
The Caballos Formation is apart from its type locality, found in Huila, Tolima and Putumayo Departments.