Jimol Formation
| Jimol Formation | |
|---|---|
| Stratigraphic range: Burdigalian (Santacrucian) ~ | |
| Type | Geological formation |
| Unit of | Cocinetas Basin |
| Underlies | Castilletes Formation |
| Overlies | Uitpa Formation |
| Thickness | up to 203 m (666 ft) |
| Lithology | |
| Primary | Sandstone |
| Other | Siltstone, mudstone |
| Location | |
| Coordinates | Lua error in Module:Coordinates at line 489: attempt to index field 'wikibase' (a nil value). |
| Region | La Guajira Caribbean region |
| Country | Colombia |
| Type section | |
| Named for | Cerro Jimol |
| Named by | Renz |
| Location | Uribia |
| Year defined | 1960 |
| Coordinates | Lua error: callParserFunction: function "#coordinates" was not found. |
| Region | La Guajira |
| Country | Colombia |
Type locality of the formation in La Guajira | |
The Jimol Formation (Spanish: Formación Jimol, N1j) is a fossiliferous geological formation of the Cocinetas Basin in the northernmost department of La Guajira. The formation consists of calcareous lithic and fossiliferous sandstones, siltstones and mudstones. The Jimol Formation dates to the Neogene period; Burdigalian stage, Santacrucian in the SALMA classification, and has a maximum thickness of 203 metres (666 ft).
Etymology
[edit | edit source]The formation was defined by Renz in 1960 and named after Cerro Jimol.[1]
Description
[edit | edit source]Lithologies
[edit | edit source]The Jimol Formation consists of calcareous lithic and fossiliferous sandstones, siltstones and mudstones.[2]
Stratigraphy and depositional environment
[edit | edit source]The Jimol Formation overlies the Uitpa Formation and is overlain by the Castilletes Formation. The age has been estimated to be Early Miocene (17.9 to 16.7 Ma), corresponding to the Santacrucian in the SALMA classification. The invertebrate fauna of the Jimol Formation is similar to the fauna found in the latest Early Miocene Cantaure Formation of Venezuela and the Culebra Formation of Panama.[3] The Jimol Formation was deposited in a beach to shallow marine environment,[4] inner shelf depth (less than 50 metres' [160 ft] water depth). This unit is correlated with the upper Agua Clara and lower Cerro Pelao Formations of the Venezuelan Falcón Basin.[5]
Petroleum geology
[edit | edit source]The Jimol Formation is a reservoir and seal rock formation in the Guajira Basin.[6]
Fossil content
[edit | edit source]See also
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- File:Cscr-candidate.svg Geology of the Eastern Hills
- File:GA candidate.svg Cesar-Ranchería Basin
- File:GA candidate.svg Honda Group
- File:Symbol start class.svg Abanico Formation
References
[edit | edit source]- ^ Moreno et al., 2015, p.7
- ^ Moreno et al., 2015, pp.18-27
- ^ a b Moreno et al., 2015, p.23
- ^ Rodríguez & Londoño, 2002, p.137
- ^ Moreno et al., 2015, p.27
- ^ ANH, 2010
- ^ a b Moreno et al., 2015, p.35
- ^ Aguilera et al., 2017, p.15
- ^ Hendy et al., 2015, p.52
- ^ Hendy et al., 2015, p.53
- ^ Hendy et al., 2015, p.54
Bibliography
[edit | edit source]Local geology
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Paleontology
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Maps
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- Geologic formations of Colombia
- Neogene Colombia
- Miocene Series of South America
- Burdigalian
- Santacrucian
- Sandstone formations
- Siltstone formations
- Mudstone formations
- Beach deposits
- Shallow marine deposits
- Reservoir rock formations
- Seal rock formations
- Fossiliferous stratigraphic units of South America
- Paleontology in Colombia
- Geography of La Guajira Department