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Tahamí Terrane

Coordinates: 7°08′00″N 75°13′45″W / 7.13333°N 75.22917°W / 7.13333; -75.22917
From Wikipedia, the free encyclopedia
Tahamí Terrane
Stratigraphic range: Permo-Triassic (emplaced)
~280–230 Ma
Tahamí Terrane is enclosed by the Bucaramanga-Santa Marta Fault (orange), northernmost Oca Fault (white) and Romeral Fault System (violet)
TypeTerrane
Unit ofNorth Andes Plate
Sub-unitsSubunits
UnderliesArquía, Caribbean, La Guajira & Quebradagrande Terranes
OverliesChibcha Terrane
Lithology
PrimaryComplexes, basins
OtherVolcanoes
Location
LocationAntioquia, Bolívar, Caldas, Cauca, La Guajira, Magdalena, Nariño, Risaralda, Sucre, Valle del Cauca departments
Coordinates7°08′00″N 75°13′45″W / 7.13333°N 75.22917°W / 7.13333; -75.22917
RegionAndean, Caribbean
Country Colombia
ExtentCentral, Macuira, SNSM
Type section
Named forTahamí [es], Nutabe
Tahamí Terrane is located in Colombia
Tahamí Terrane
Tahamí Terrane (Colombia)
Tahamí Terrane is located in Antioquia Department
Tahamí Terrane
Tahamí Terrane (Antioquia Department)

The Tahamí (Spanish: Terreno Tahamí, TT) or Tahamí-Panzenú Terrane is one of the geological provinces (terranes) of Colombia. The terrane, dating to the Permo-Triassic, is situated on the North Andes Plate. The contact with the Chibcha, Arquía and Quebradagrande Terranes is formed by the megaregional Romeral Fault System.[1] A tiny terrane is located at the contact with the Quebradagrande Terrane; Anacona Terrane.[2]

The terrane is offset along the regional Bucaramanga-Santa Marta Fault from the Caribbean, La Guajira and Chibcha Terranes,[3] and by the regional Oca Fault with the Chibcha Terrane.[4]

Etymology

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Geologic map of Colombia, Venezuela and Ecuador
(Codazzi, 1890)

The terrane is, as the Chibcha Terrane, named after an indigenous people from Antioquia; the Chibcha-speaking Tahamí [es], part of the greater Nutabe group. Panzenú refers to the Zenú civilization, that thrived from about 200 BCE to 1600 CE in the Sinú river basin.

Reinterpretation

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A study performed by Mora Bohórquez et al. in 2017 showed no basement variation between the Chibcha Terrane San Lucas basement underlying the Lower Magdalena Valley (VIM) and the SNSM basement to the east of the Santa Marta Fault. The authors redefined the contacts between the different terranes, using the names Calima Terrane for the coastal portion of the Caribbean Terrane (San Jacinto and Sinú foldbelts) and Tahamí-Panzenú Terrane for the Tahamí Terrane.[5]

Subdivision

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Complexes

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Volcanoes

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Ranges

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Basins

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Faults

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bounding faults in bold

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See also

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References

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  1. ^ a b Paris et al., 2000, pp.20–26
  2. ^ Gómez Tapias et al., 2015, p.209
  3. ^ a b Paris et al., 2000, p.10
  4. ^ Paris et al., 2000, p.9
  5. ^ a b Mora Bohórquez et al., 2017, p.20
  6. ^ a b Paris et al., 2000, p.29
  7. ^ a b Paris et al., 2000, p.30
  8. ^ Paris et al., 2000, p.49
  9. ^ Paris et al., 2000, p.31
  10. ^ Paris et al., 2000, p.28
  11. ^ Paris et al., 2000, p.27

Bibliography

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Terranes

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  • Gómez Tapias, Jorge; Montes Ramírez, Nohora E.; Almanza Meléndez, María F.; Alcárcel Gutiérrez, Fernando A.; Madrid Montoya, César A.; Diederix, Hans (2015), Geological Map of Colombia, Servicio Geológico Colombiano, pp. 1–212, retrieved 2019-10-29
  • Restrepo, Jorge Julián; Ordóñez Carmona, Oswaldo; Martens, Uwe; Correa, Ana María (2009), "Terrenos, complejos y provincias en la Cordillera Central de Colombia (Terrains, complexes and provinces in the central cordillera of Colombia)", Ingeniería Investigación y Desarrollo, 9: 49–56, retrieved 2019-10-31
  • Cordani, U.G.; Cardona, A.; Jiménez, D.M.; Dunyl, L.; Nutman, A.P. (2003), Geochronology of Proterozoic basement from the Colombian Andes: Tectonic history of remnants from a fragmented Grenville Belt, 10o Congreso Geológico Chileno, pp. 1–10
  • Restrepo, Jorge Julian; Toussaint, Jean F. (1988), "Terranes and continental accretion in the Colombian Andes", Episodes, 11 (3): 189–193, doi:10.18814/epiiugs/1988/v11i3/006, retrieved 2019-10-31

Tahamí Terrane

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Reports

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Maps

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