Guavio Formation

Guavio Formation
Stratigraphic range: Tithonian-Berriasian
~150–140 Ma

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Guavio Formation; Stratigraphic range: Tithonian-Berriasian; ~150–140 Ma PreЄ Є O S D C P T J K Pg N
Type	Geological formation
Unit of	Cáqueza Group
Sub-units	Caliza de Las Mercedes Mb.; Lutitas de Las Mercedes Mb.; Caliza de Malacara Mb.; Lutitas de Miralindo Mb.; Conglomerado de Miralindo
Underlies	Macanal Formation
Overlies	Batá Fm., Girón Fm
Thickness	up to 1,000 m (3,300 ft)
Lithology
Primary	Conglomerate
Other	Limestone, shale
Location
Coordinates	4°59′34.1″N 73°28′53.8″W / 4.992806°N 73.481611°WCoordinates: 4°59′34.1″N 73°28′53.8″W / 4.992806°N 73.481611°W
Region	Altiplano Cundiboyacense; Eastern Ranges, Andes
Country	Colombia
Type section
Named for	Guavio River
Named by	Rodríguez & Ulloa
Location	Alto de Miralindo, Guateque
Year defined	1976
Coordinates	4°59′34.1″N 73°28′53.8″W / 4.992806°N 73.481611°W
Region	Cundinamarca, Boyacá
Country	Colombia
	; Paleogeography of Northern South America; 150 Ma, by Ron Blakey

The Guavio Formation (Spanish: Calizas del Guavio, Kicg) is a geological formation of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consists of conglomerates, shales and limestones, dates to the Late Jurassic and Early Cretaceous periods; Tithonian to Berriasian epochs and has a maximum thickness of 1,000 metres (3,300 ft).

Etymology

The formation was defined and named in 1976 by Rodríguez and Ulloa after the Guavio River, Cundinamarca.^[1]

Description

Lithologies

The Guavio Formation has a maximum thickness of 1,000 metres (3,300 ft), and is characterised by a sequence of conglomerates, shales and limestones.^[1]

Stratigraphy and depositional environment

The Guavio Formation, the lowermost unit of the Cáqueza Group, overlies the Batá Formation and is overlain by the Macanal Formation. The unit is subdivided into five members, from old to younger; Conglomerado de Miralindo, Lutitas de Miralindo, Caliza de Malacara, Lutitas de Las Mercedes and Caliza de Las Mercedes. The age has been estimated to be Tithonian to Berriasian, spanning the Jurassic-Cretaceous boundary. Stratigraphically, the formation is time equivalent with the Arcabuco Formation. The formation has been deposited in a shallow marine environment in an oxygen-poor basin.^[1]

Outcrops

Type locality of the Guavio Formation to the east of the Altiplano Cundiboyacense

The Guavio Formation is apart from its type locality at the Alto de Miralindo and Cuchilla de Manizales, found near Gachalá and Medina.^[1]

Regional correlations

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

References

1 2 3 4 Acosta & Ulloa, 2002, p.51

Bibliography

Acosta Garay, Jorge E., and Carlos E. Ulloa Melo. 2002. Mapa Geológico del Departamento de Cundinamarca - 1:250,000 - Memoria explicativa, 1–108. INGEOMINAS. Accessed 2017-04-26.
García González, Mario; Ricardo Mier Umaña; Luis Enrique Cruz Guevara, and Mauricio Vásquez. 2009. Informe Ejecutivo - evaluación del potencial hidrocarburífero de las cuencas colombianas, 1-219. Universidad Industrial de Santander.
Villamil, Tomas. 2012. Chronology Relative Sea Level History and a New Sequence Stratigraphic Model for Basinal Cretaceous Facies of Colombia, 161–216. Society for Sedimentary Geology (SEPM).

Maps

Acosta, Jorge E, and Carlos E. Ulloa. 1998. Plancha 246 - Geología de Fusagasugá - 1:100,000, 1. INGEOMINAS.
Ulloa, Carlos E; Erasmo Rodríguez, and Jorge E. Acosta. 1998. Plancha 227 - Geología de La Mesa - 1:100,000, 1. INGEOMINAS.
Ulloa, Carlos E; Erasmo Rodríguez, and Ricardo Escovar. 1998. Plancha 192 - Geología de Laguna de Tota - 1:100,000, 1. INGEOMINAS.
Renzoni, Giancarlo; Humberto Rosas, and Fernando Etayo Serna. 1998. Plancha 191 - Geología de Tunja - 1:100,000, 1. INGEOMINAS.
Fuquen M., Jaime A, and José F. Osorno M. 2009. Plancha 190 - Geología de Chiquinquirá - 1:100,000, 1. INGEOMINAS.
Ulloa, Carlos E; Álvaro Guerra, and Ricardo Escovar. 1998. Plancha 172 - Geología de Paz de Río - 1:100,000, 1. INGEOMINAS.
Velandia, Francisco, and Héctor Cepeda. 2005. Planchas 171 & 191 - Geología sector del sur del municipio de Paipa (Boyacá) - 1:25,000. INGEOMINAS.

External links

Gómez, J.; N.E. Montes; Á. Nivia, and H. Diederix. 2015. Plancha 5-09 del Atlas Geológico de Colombia 2015 – escala 1:500,000, 1. Servicio Geológico Colombiano. Accessed 2017-03-16.

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[Acosta2002_p51-1] 1 2 3 4 Acosta & Ulloa, 2002, p.51