Earth:Río Cachirí Group

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Short description: Geological group in the Venezuelan Andes
Río Cachirí Group
Stratigraphic range: Devonian
419–360 Ma
TypeGeological group
Unit ofCesar-Ranchería Basin, Serranía del Perijá
Sub-unitsCaño Grande Fm., Caño del Oeste Fm., Campo Chico Fm., Los Guineos Fm.
UnderliesCarboniferous sequence
OverliesPerijá Formation
Thickness~1,100 m (3,600 ft) (Colombia)
2,438 m (7,999 ft) (Venezuela)
Lithology
PrimaryShale, sandstone
OtherLimestone
Location
Coordinates [ ⚑ ] : 10°50′03″N 72°14′23″W / 10.83417°N 72.23972°W / 10.83417; -72.23972
RegionCesar, La Guajira
Zulia
Country Colombia
 Venezuela
Extent~110 km (68 mi) (Venezuela)
Type section
Named forRío Cachirí
Named byLiddle
LocationMara
Year defined1928
Coordinates [ ⚑ ] 10°50′03″N 72°14′23″W / 10.83417°N 72.23972°W / 10.83417; -72.23972
RegionZulia
Country Venezuela
Thickness at type section2,438 m (7,999 ft)
380 Ma plate tectonic reconstruction.png
Paleogeography of the Middle Devonian
380 Ma, by Stampfli & Borel

The Río Cachirí Group (Spanish: Grupo Río Cachirí, PZc) is a geological group of the Cesar-Ranchería Basin, Colombia and the Serranía del Perijá of the northernmost Colombian and Venezuelan Andes. The group of shales, sandstones and limestones is of Devonian age and has a maximum thickness in the Venezuelan section of 2,438 metres (7,999 ft). The group contains abundant fauna; crinoids, bryozoa, brachiopods and molluscs have been found in the group.

Etymology and definition

The formation was defined by Liddle in 1928 in Río Cachirí, part of Mara, Zulia, in the Venezuelan part of the Serranía del Perijá, and the same author subdivided the group into three formations in 1943. In 1972, Bowen added a fourth formation to the group.[1]

Description

Lithologies

The group contains black, grey and red shales, grey micaceous sandstones, quartzitic sandstones and red and bluish grey limestones.[1]

Stratigraphy and correlation

The Río Cachirí Group, dated to span the Devonian, is subdivided into the Caño Grande, Caño del Oeste, Campo Chico and Los Guineos Formations. The maximum thickness has been recorded in Venezuela, with 2,438 metres (7,999 ft), while the thickness on the Colombian side of the range does not exceed 1,100 metres (3,600 ft).[1] The group is recognised along a section of approximately 110 kilometres (68 mi) in the Venezuelan terrain.[2] The group unconformably overlies the Perijá Formation and is overlain by an unnamed Carboniferous sequence. The Río Cachirí Group is time-equivalent with the Floresta and Cuche Formations of the Floresta Massif, Altiplano Cundiboyacense and the Quetame Group of the Eastern Ranges.[3] The sediments of the Río Cachirí Group were deposited in an epicontinental sea at the edge of the Paleo-Tethys Ocean.[1]

Fossil content

The group contains abundant fossils of crinoids, bryozoa, brachiopods and molluscs as Acrospirifer olssoni, Spirifer kingi, Leptaena boyaca, Fenestella venezuelansis, Neospirifer latus, Composita subtilita, Phricodrotis planoconvexa and Pecten sp.[4]

Outcrops

Río Cachirí Group is located in Venezuela
Río Cachirí Group
Type locality of the Río Cachirí Group in Venezuela

Apart from its type locality on the eastern flank of the Serranía del Perijá in Zulia, Venezuela, the formation is also found in other parts of the mountain range, on the Colombian western side in the east of San Diego and Curumaní, Cesar.[5][6]

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

Notes

References

  1. 1.0 1.1 1.2 1.3 Ayala, 2009, p.20
  2. Hernández Ferrer, 2011, p.47
  3. Ayala, 2009, p.21
  4. García González et al., 2007, p.68
  5. Plancha 34, 2007
  6. Plancha 48, 2008

Bibliography

Maps