Earth:Simijaca Formation

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Simijaca Formation
Stratigraphic range: Cenomanian-Turonian
~100–90 Ma
TypeGeological formation
Unit ofVilleta Group
UnderliesLa Frontera Formation
OverliesChiquinquirá Sst., Churuvita Fm., Hiló Fm., Pacho Fm.
Thicknessup to 693 m (2,270 ft)
Lithology
PrimaryMudstone
OtherShale, sandstone, limestone
Location
Coordinates [ ⚑ ] : 5°29′15″N 73°50′55″W / 5.4875°N 73.84861°W / 5.4875; -73.84861
RegionAltiplano Cundiboyacense
Eastern Ranges, Andes
Country Colombia
Type section
Named forSimijaca
Named byUlloa & Rodríguez
LocationSouth of Simijaca
Year defined1991
Coordinates [ ⚑ ] 5°29′15″N 73°50′55″W / 5.4875°N 73.84861°W / 5.4875; -73.84861
RegionCundinamarca, Boyacá
Country Colombia
Thickness at type section432 metres (1,420 ft)
Blakey 090Ma - COL.jpg
Paleogeography of Northern South America
90 Ma, by Ron Blakey

The Simijaca Formation (Spanish: Formación Simijaca, K2S, Kss) is a geological formation of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The predominantly mudstone formation dates to the Late Cretaceous period; Turonian and Cenomanian epochs, and has a maximum thickness of 693 metres (2,274 ft).

Etymology

The formation was defined and named in 1991 by Ulloa and Rodríguez after Simijaca, Cundinamarca.[1]

Description

Lithologies

The Simijaca Formation is characterised by a sequence of mudstones, grey and black shales with sandstone and limestone intercalations.[1][2]

Stratigraphy and depositional environment

The Simijaca Formation conformably overlies the Chiquinquirá Sandstone, and the Hiló and Pacho Formations, and is overlain by the La Frontera Formation.[3] The age has been estimated to be Turonian,[1] or Cenomanian.[4] Stratigraphically, the formation is time equivalent with the Chipaque Formation.[5] The formation has been deposited in an open marine platform setting.[6] The deposition is represented by a maximum flooding surface.[7]

Outcrops

Lua error in Module:Location_map at line 522: Unable to find the specified location map definition: "Module:Location map/data/Altiplano Cundiboyacense" does not exist. The Simijaca Formation is apart from its type locality in the Quebrada Don Lope,[2] found at surface in the north of the Bogotá savanna, in the Tabio anticlinal, along the road Ubaté-Carmen de Carupa,[8] at the western and eastern flanks of the Aponsentos-Chiquinquirá Synclinal,[9] near Tena, south of Anolaima and Cachipay,[10] and between Anapoima and Granada.[11]

Regional correlations

See also

Featured article candidate Geology of the Eastern Hills
B-Class article Geology of the Ocetá Páramo
C-Class article Geology of the Altiplano Cundiboyacense

References

  1. 1.0 1.1 1.2 Montoya & Reyes, 2005, p.21
  2. 2.0 2.1 Acosta & Ulloa, 2001, p.38
  3. Acosta & Ulloa, 2001, p.32
  4. Acosta & Ulloa, 2001, p.41
  5. Montoya & Reyes, 2005, p.22
  6. García González et al., 2009, p.209
  7. Villamil, 2012, p.164
  8. Montoya & Reyes, 2005, p.23
  9. Plancha 190, 2009
  10. Plancha 227, 1998
  11. Plancha 246, 1998

Bibliography

  • Acosta Garay, Jorge, and Carlos E. Ulloa Melo. 2001. Geología de la Plancha 208 Villeta - 1:100,000, 1-84. INGEOMINAS. Accessed 2017-03-23.
  • 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.
  • Montoya Arenas, Diana María, and Germán Alfonso Reyes Torres. 2005. Geología de la Sabana de Bogotá, 1–104. INGEOMINAS.
  • 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

External links