Girón Formation
The Girón Formation (Spanish: Formación Girón, Jg) is an extensive geological formation stretching across 325 kilometres (202 mi) from the north in Teorama, Norte de Santander, across the Mesa de Los Santos and Chicamocha Canyon towards west of Nobsa, Boyacá in the northern part of the Altiplano Cundiboyacense in the south. The formation extends across the northern and central part of the Eastern Ranges of the Colombian Andes.
| Girón Formation | |
|---|---|
| Stratigraphic range: Late Jurassic ~ | |
| Type | Geological formation |
| Underlies | Rosablanca, Río Negro, Tambor & Tibú-Mercedes Formations |
| Overlies | Bucaramanga Gneiss, Arboleda Granite, Diamante, Floresta, Bocas & Jordán Formations |
| Thickness | Up to 3,346 m (10,978 ft) |
| Lithology | |
| Primary | Sandstone, siltstone, conglomerate |
| Other | Shale, claystone, rhyolite, tuff |
| Location | |
| Location | Mesa de Los Santos & Altiplano Cundiboyacense Eastern Ranges, Andes |
| Coordinates | 6°46′17″N 73°02′30″W / 6.77139°N 73.04167°W |
| Region | Santander, Norte de Santander, Boyacá |
| Country | Colombia |
| Extent | 325 km (202 mi) |
| Type section | |
| Named for | Girón |
| Named by | Hettner (1892) Langenheim |
| Location | Lebrija River |
| Year defined | 1954 |
| Coordinates | 7°11′39″N 74°09′13″W / 7.19417°N 74.15361°W |
| Region | Santander |
| Country | Colombia |
| Thickness at type section | 3,346 m (10,978 ft) |
Paleogeography of Northern South America 150 Ma, by Ron Blakey | |
The formation forms the basement in the Middle Magdalena Valley and is forming the Serranía de Los Cobardes. The Girón Formation consists of thickly bedded red sandstones, shales, siltstones and conglomerates deposited in a terrestrial alluvial and fluvial to fluvio-lacustrine environment in an extensional basin setting. The formation dates to the Late Jurassic period and has a maximum thickness of 3,346 metres (10,978 ft) at its type locality in the valley of the Lebrija River.
Definition edit
The formation was first defined by Hettner in 1892 and named after Girón, close to Bucaramanga, Santander. The type locality was defined by Langenheim in 1954 in the valley of the Lebrija River. The formation was studied by various authors in the 1940s, Oppenheim in 1940, Dickey in 1941 and Trumpy in 1943, who described the formation as a lateral equivalent of the La Quinta Formation of northern Colombia and western Venezuela. Julivert (1958) assigned a thickness of 2,500 metres (8,200 ft), while Navas in 1963 observed a thickness of 2,690 metres (8,830 ft). Cediel in the same year defined the thickness at its type locality of 4,650 metres (15,260 ft) and divided the formation in seven units.[1] Research by Osorio and Velandia, published in 2015, concluded a maximum thickness of 3,346 metres (10,978 ft) at the type locality.[2] On the Cáchira Páramo in Norte de Santander, the thickness is 1,140 metres (3,740 ft).[3]
Description edit
The Girón Formation extends over a distance of about 325 kilometres (202 mi) from Teorama in Norte de Santander in the north to Nobsa in Boyacá in the south, stretching across three departments; Norte de Santander, Santander and Boyacá.
Lithologies edit
The Girón Formation is characterized by a thick sequence of red feldspathic and micaceaous sandstones and thinly bedded reddish siltstones, conglomerates with quartz and lithic clasts, shales with white spots and purple to dark red claystones. In the south, the formation includes fragments of schists, quartzites, and red and green limonite.[1] The middle part of the sequence contains alternating greyish green sandstones and red to purple siltstones in beds up to 1.5 metres (4.9 ft).[4] In the Middle Magdalena Valley (VMM), the Girón Formation has been drilled and proved to comprise rhyolitic, rhyodacitic flows and tuffs.[5] To the southeast of Cáchira, Norte de Santander, andesitic porphyry copper deposits in mineralizations of chalcopyrite and bornite occur in the Girón Formation.[6]
Stratigraphy and depositional environment edit
The Girón Formation in large areas of its extent overlies the Precambrian Bucaramanga Gneiss,[7] in the northern area the Arboleda Granite,[8] and the Carboniferous to Permian Diamante Formation in the area around Toledo, Norte de Santander.[9] In this part, the formation is overlain by the Río Negro and Tibú-Mercedes Formations.[4]
In the central area at the type locality in the Lebrija River valley, the formation unconformably overlies the Bocas Formation and is overlain by the Tambor Formation.[1] On the Mesa de Los Santos and the Bucaramanga Massif, the formation overlies the Jordán Formation with an angular unconformity dipping 10 to 15°.[10] In the central part it is overlain by the Rosablanca Formation. In the southernmost extent of the formation, along the road from Busbanzá to Corrales, the Girón Formation unconformably rests upon the Floresta Formation.[11] The formation forms the economic basement in the Middle Magdalena Valley.[5]
The age has been estimated to be Late Jurassic, ranging from Oxfordian to Tithonian,[12] based on ostracods and palynomorphs.[10] Stratigraphically, the formation is time equivalent with the Buena Vista Breccia of the proximal area of the Llanos Basin and the Arcabuco Formation to the west of the Boyacá Fault.[13]
The formation was deposited in an alluvial to fluvial or fluvio-lacustrine terrestrial environment,[4] with fast-flowing braided rivers and in certain parts meandering river deposition to a deltaic environment. Towards the top of the stratigraphic unit, the deposition became shallow marine.[14] The overall tectonic regime represented an extensional basin setting.[15] The rifting of the Jurassic and Early Cretaceous, resulting from the break-up of Pangea, caused large variations in thickness of the Girón Formation.[16]
Provenance edit
The grains composing the Girón Formation have been analyzed using X-ray diffraction, resulting in quartz as principal component (73 to 97%), and clay minerals belonging to the kaolinite group (2 to 4%) and illite-mica (3-19%). It has been suggested a main component of the provenance for the sediments was the Devonian Floresta Formation.[17]
Tectonics edit
class=notpageimage| Norte de Santander | class=notpageimage| Santander |
| Extent of the Girón Formation Northernmost outcrop in Teorama, Norte de Santander Type locality at the Lebrija River, Santander Outcrop in the Chicamocha Canyon, Santander Southernmost outcrop in Nobsa, Boyacá | |
The Girón Formation probably deposited as a result of regional uplift of the Santander and Floresta Massifs in the Late Jurassic.[18] The formation is folded in an anticline around the type locality producing the Los Cobardes Anticlinal that extends to Contratación.[19][20][21] Transpressive tectonic movements after deposition produced five sets of fractures; an asymmetrical group of NW-SE, NW-SE, and E-W fractures and a set symmetrical with the general anticline at NNE-SSW and ESE-WNW.[2] Pervasive cleavage exists in the formation at the Floresta Massif.[22] Magnetization analysis performed in 2005 by Ayala et al. showed clockwise rotation of the formation in the southern area around Paz de Río of 31 ± 18° and Nobsa of 40 ± 18° respectively.[23] The Girón Formation is put into contact with the Cretaceous La Luna Formation in Norte de Santander,[24] and is present in the hanging wall of the Bituima-La Salina Fault and cross-cut by several faults, among which the Suárez, Cáchira,[25][26] and the regional Bucaramanga-Santa Marta Fault.[27][28]
Outcrops edit
The Girón Formation is found, apart from its type locality in the Lebrija River valley in Santander, stretching from the north around Teorama, Norte de Santander,[29] to the south west of Nobsa in Boyacá.[30] The formation crops out along the Colombia-Venezuela border in Toledo, Norte de Santander,[31] and the urban center of Hacarí is built on top of the Girón Formation.[32] The formation forms the Serranía de Los Cobardes in the western front of the Eastern Ranges and is found throughout the Chicamocha Canyon,[33][34] and the Sogamoso River cuts through the Girón Formation.[28]
The Girón Formation also crops out along the highway from Bucaramanga to Piedecuesta where frequent landslides of the fractured rocks occur in the rainy season.[35][36][37]
See also edit
References edit
- ^ a b c Pulido González, 1985, p.9
- ^ a b Osorio & Velandia, 2015, p.979
- ^ Fúquen et al., 2011, p.43
- ^ a b c Royero Gutiérrez, 2001, p.16
- ^ a b Garavito Cubillos, 2008, p.31
- ^ Fúquen, 2011, p.105
- ^ Royero Gutiérrez, 2001, p.13
- ^ Fúquen, 2011, p.46
- ^ Royero Gutiérrez, 2001, p.15
- ^ a b Ayala et al., 2005, p.50
- ^ Ulloa et al., 2003, p.45
- ^ Méndez Espinosa, 2017, p.33
- ^ Méndez Espinosa, 2017, p.32
- ^ Fúquen, 2011, p.45
- ^ Fúquen et al., 2011, p.15
- ^ Jiménez et al., 2016, p.318
- ^ Méndez Espinosa, 2017, p.147
- ^ Mojica & Kammer, 1995, p.170
- ^ Osorio & Velandia, 2015, p.975
- ^ Jiménez et al., 2016, p.314
- ^ Plancha 151, 2009
- ^ Ayala et al., 2005, p.53
- ^ Ayala et al., 2005, p.62
- ^ Fúquen, 2011, p.77
- ^ Plancha 86, 1981
- ^ Plancha 97, 2009
- ^ Jiménez et al., 2016, p.315
- ^ a b Plancha 120, 2010
- ^ Plancha 66, 2009
- ^ Plancha 172, 1998
- ^ Plancha 111, 1999
- ^ Plancha 76, 2009
- ^ Plancha 135, 2009
- ^ Plancha 136, 1984
- ^ Taponada Vía Bucaramanga-Bogotá - 1984 - El Tiempo
- ^ Derrumbes en Piedecuesta en Santander tienen incomunicadas a dos veredas - 2017 - RCN Radio
- ^ Enormes derrumbes taponan cuatro ejes viales de Santander. Paso restringido a un carril - 2018 - El Frente
Bibliography edit
- Ayala Calvo, Rosa Carolina; Gabriel Eduardo Veloza Fajardo; Germán Bayona; Mayeli Gómez Casallas; Augusto Ernesto Rapalini; Vincenzo Costanzo Álvarez; Milagrosa Aldana, and Martin Cortés. 2005. Paleomagnetísmo y Mineralogía Magnética en las unidades del Mesozoico de Bucaramanga y el Macizo de Floresta. Geología Colombiana 30. 49–66. Accessed 2018-10-09.
- Fúquen M., Jaime A.; Leonardo Ceballos; Edwin Marín; Alejandro Patiño, and Andrea Pedraza. 2011. Geología de las Planchas 98 Durania y 99 Villa del Rosario, Norte de Santander - Colombia, 1–119. INGEOMINAS. Accessed 2018-10-09.
- Garavito Cubillos, Flavio. 2008. Structural analysis of an area in the northern central part of the Middle Magdalena Valley Basin, Colombia, 1–105. Colorado School of Mines. Accessed 2018-10-09.
- Jiménez, Giovanny; Oscar López; Leonardo Jaimes, and Ricardo Mier Umaña. 2016. Variaciones en el estilo estructural relacionado con anisotropias de basamento en el Valle Medio del Magdalena. Revista de la Academia Colombiana de Ciencias Exactas, Físicas y Naturales 40. 312–319. Accessed 2018-10-09.
- Méndez Espinosa, Sandra Catalina. 2017. Análisis de procedencia de rocas siliciclásticas de las formaciones Girón y Tibasosa en el Macizo de Floresta (MSc. thesis), 1–219. Universidad Nacional de Colombia.
- Mojica, Jairo, and Andreas Kammer. 1995. Eventos Jurásicos en Colombia. Geología Colombiana 19. 165–172. Accessed 2018-10-09.
- Osorio, Diego, and Francisco Velandia. 2015. Espesor estratigráfico medido y análisis de fracturas en la sección tipo de la Formación Girón (Río Lebrija), 975–979. XV Congreso Colombiano de Geología, Bucaramanga. Accessed 2018-10-09.
- Pulido González, Orlando. 1985. Reseña explicativa del mapa geológico preliminar de la Plancha 135 San Gil 1:100,000, 1–24. INGEOMINAS. Accessed 2018-10-09.
- Royero Gutiérrez, José María. 2001. Geología y geoquímica de la Plancha 111 Toledo - Norte de Santander 1:100,000, 1–56. INGEOMINAS.
- Ulloa, Carlos; Erasmo Rodríguez, and Gloria Inés Rodríguez. 2003. Memoria Explicativa de la Plancha 172 Paz de Río 1:100,000, 1–109. INGEOMINAS.
Maps edit
- Royero Gutiérrez, José María, and Rodrigo Vargas Higuera. 1999. Mapa Geológico de Santander 1:300,000, 1. INGEOMINAS. Accessed 2018-10-09.
- Daconte, Rommel; Rosalba Salinas; José María Royero; Jairo Clavijo; Alfonso Arias; Luz S. Carvajal; Martín E. López; Leonidas Angarita, and Hernando Mendoza. 2009. Plancha 66 - Miraflores - 1:100,000, 1. INGEOMINAS. Accessed 2018-10-09.
- Daconte, Rommel, and Rosalba Salinas. 1980. Plancha 76 - Ocaña - 1:100,000, 1. INGEOMINAS. Accessed 2018-10-09.
- Vargas, Rodrigo, and Alfonso Arias. 1981. Plancha 86 - Ábrego - 1:100,000, 1. INGEOMINAS. Accessed 2018-10-09.
- Vargas, Rodrigo, and Alfonso Arias. 2009. Plancha 97 - Cáchira - 1:100,000, 1. INGEOMINAS. Accessed 2018-10-09.
- Royero, José María; J. Zambrano; Rommel Daconte; H. Mendoza, and Rodrigo Vargas. 1999. Plancha 111 - Toledo - 1:100,000, 1. INGEOMINAS. Accessed 2018-10-09.
- Ward, Dwight E.; Richard Goldsmith; Andrés Jimeno; Jaime Cruz; Hernán Restrepo, and Eduardo Gómez. 2010. Plancha 120 - Bucaramanga - 1:100,000, 1. INGEOMINAS. Accessed 2018-10-09.
- Angarita, Leonidas; Víctor Carrillo; Alfonso Castro; Rommel Daconte; Mario Niño; Orlando G. Pulido; J. Antonio Rodríguez; José María Royero, and Rosalba Salinas, Carlos Ulloa and Rodrigo Vargas. 2009. Plancha 135 - San Gil - 1:100,000, 1. INGEOMINAS. Accessed 2018-10-09.
- Vargas, Rodrigo; Alfonso Arias; Luis Jaramillo, and Noel Tellez. 1984. Plancha 136 - Málaga - 1:100,000, 1. INGEOMINAS. Accessed 2018-10-09.
- Pulido González, Orlando. 2009. Plancha 151 - Charalá - 1:100,000, 1. INGEOMINAS. Accessed 2018-10-09.
- Ulloa, Carlos E.; Álvaro Guerra, and Ricardo Escovar. 1998. Plancha 172 - Paz de Río - 1:100,000, 1. INGEOMINAS. Accessed 2018-10-09.