Trincheras Formation
# Trincheras Formation

The Trincheras Formation (Spanish: Formación Trincheras, Kitr) is a geological formation of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consisting of a lower unit of calcareous shales and an upper sequence of shales dates to the Early Cretaceous period; Early Aptian epoch and has a maximum thickness of 1,260 metres (4,130 ft). The formation, deposited in a marine platform environment, part of a transgressive cycle, hosts ammonite, bryozoan, mollusc and echinoid fossils.

## Etymology

The formation was defined and named in 1969 by Cáceres and Etayo after Quebrada Trincheras, Apulo, Cundinamarca.

## Description

### Lithologies

The Trincheras Formation has a maximum thickness of 1,260 metres (4,130 ft), and is characterised by a sequence of claystones with intercalated limestones and sandstones. Fossils of the ammonites Heinzia sp., Pseudohaploceras sp., Heminautilus etheringtoni, Cheloniceras sp. and bryozoans, molluscs and echinoids have been found in the Trincheras Formation.

### Stratigraphy and depositional environment

The Trincheras Formation is the lowermost unit of the Villeta Group, and conformably overlies the Murca, La Naveta and Útica Formations. The formation is overlain in a transitional pattern by the Socotá and El Peñón Formations. The Trincheras Formation is subdivided into the El Tigre and Anapoima Members. The age has been estimated to be Early Aptian. Stratigraphically, the formation is time equivalent with the fossiliferous Paja Formation of Boyacá and the Las Juntas Formation. The formation has been deposited in a marine well oxygenated platform environment. In terms of sequence stratigraphy, this phase was transgressional.

## Outcrops

The Trincheras Formation is apart from its type locality in Apulo, found near La Mesa and Anapoima, in the Villeta Anticlinal, the Murca-Guayabal-Nimaima Anticlinal and along the roads between Pacho and La Palma and Útica-La Peña. The formation also crops out around San Joaquín east of La Mesa, and on the right bank of the Bogotá River near Apulo.

The reverse Bituima Fault thrusts the Trincheras Formation on top of the Güagüaquí Group, while the Bogotá River Fault laterally displaces the formation near Anapoima.

## Regional correlations

Cretaceous stratigraphy of the central Colombian Eastern Ranges :

| Age | VMM | Guaduas-Vélez | Guaduas-Vélez | W Emerald Belt | W Emerald Belt | Villeta anticlinal | Villeta anticlinal | Chiquinquirá- Arcabuco | Tunja- Duitama | Altiplano Cundiboyacense | Altiplano Cundiboyacense | El Cocuy |
| - | - | - | - | - | - | - | - | - | - | - | - | - |
| Maastrichtian | Umir | Córdoba | Córdoba | Seca | Seca | eroded | eroded | Guaduas | Guaduas | Guaduas | Guaduas | Colón-Mito Juan |
| Maastrichtian | Umir | Córdoba | Córdoba | Umir | Umir | eroded | eroded | Guadalupe | Guadalupe | Guadalupe | Guadalupe | | | | Colón-Mito Juan |
| Campanian | Umir | Córdoba | Córdoba | Córdoba | Córdoba | | eroded | eroded | Guadalupe | Guadalupe | Guadalupe | Guadalupe | Colón-Mito Juan |
| Colón-Mito Juan ||
| Santonian | La Luna | Cimarrona - La Tabla | Cimarrona - La Tabla | Oliní | Oliní | eroded | eroded | Guadalupe | Guadalupe | Guadalupe | Guadalupe | La Luna |
| Coniacian | La Luna | Oliní | Oliní | Oliní | Oliní | Villeta | Conejo | Conejo | Chipaque | Chipaque | Chipaque | | | La Luna |
| Coniacian | La Luna | Güagüaquí | Loma Gorda | undefined | undefined | Villeta | La Frontera | La Frontera | | Chipaque | Chipaque | Chipaque | La Luna |
| Turonian | La Luna | Güagüaquí | Hondita | La Frontera | Otanche | Villeta | La Frontera | La Frontera | Chipaque | Chipaque | Chipaque | La Luna |
| Cenomanian | Simití | hiatus | hiatus | La Corona | Otanche | Villeta | Simijaca | Simijaca | Chipaque | Chipaque | Chipaque | Capacho |
| Cenomanian | Simití | hiatus | hiatus | Pacho Fm. | Otanche | Villeta | Hiló - Pacho | Churuvita | Une | Une | Une | Aguardiente |
| Albian | Simití | hiatus | hiatus | Hiló | Otanche | Villeta | Hiló - Pacho | Chiquinquirá | Tibasosa | Une | Une | | Aguardiente |
| Albian | Tablazo | hiatus | hiatus | Tablazo | Tablazo | Villeta | Capotes - La Palma - Simití | Simití | Tibasosa | Une | Une | Tibú-Mercedes |
| Aptian | Tablazo | hiatus | hiatus | Capotes | Capotes | Villeta | Socotá - El Peñón | Paja | Tibasosa | Fómeque | Fómeque | | Tibú-Mercedes |
| Aptian | Paja | hiatus | hiatus | Paja | El Peñón | Villeta | Trincheras | Paja | Tibasosa | Fómeque | Fómeque | Río Negro |
| Río Negro ||
| Barremian | Paja | hiatus | hiatus | Paja | El Peñón | La Naveta | La Naveta | Paja | Tibasosa | Fómeque | Fómeque | Río Negro |
| Hauterivian | Paja | hiatus | hiatus | Paja | Muzo | La Naveta | La Naveta | Paja | Tibasosa | Cáqueza | Las Juntas | Río Negro |
| Hauterivian | Rosablanca | hiatus | hiatus | Paja | Muzo | La Naveta | La Naveta | Ritoque | Tibasosa | Cáqueza | Las Juntas | Río Negro |
| Valanginian | Rosablanca | hiatus | hiatus | Ritoque | Furatena | Útica - Murca | Útica - Murca | Rosablanca | hiatus | Cáqueza | Macanal | Río Negro |
| Valanginian | Rosablanca | hiatus | hiatus | Rosablanca | Furatena | Útica - Murca | Útica - Murca | Rosablanca | hiatus | Cáqueza | Macanal | Río Negro |
| Berriasian | Cumbre | hiatus | hiatus | Cumbre | Cumbre | Útica - Murca | Útica - Murca | Los Medios | hiatus | Cáqueza | Guavio | Río Negro |
| Berriasian | Tambor | hiatus | hiatus | Arcabuco | Arcabuco | Útica - Murca | Útica - Murca | Cumbre | hiatus | Cáqueza | Guavio | Río Negro |
| Sources ||||||||||||||
