Earth:Pacho Formation

From HandWiki
Pacho Formation
Stratigraphic range: Late Albian-Cenomanian
~102–97 Ma
TypeGeological formation
Unit ofVilleta Group
UnderliesSimijaca Formation
OverliesHiló Formation
Thickness~1,050 m (3,440 ft)
Lithology
PrimarySiltstone
OtherShale
Location
Coordinates [ ⚑ ] : 4°27′07″N 74°03′20″W / 4.45194°N 74.05556°W / 4.45194; -74.05556
RegionAltiplano Cundiboyacense
Eastern Ranges, Andes
Country Colombia
Type section
Named forPacho
Named byUlloa
LocationPacho
Year defined1982
Coordinates [ ⚑ ] 4°27′07″N 74°03′20″W / 4.45194°N 74.05556°W / 4.45194; -74.05556
RegionCundinamarca
Country Colombia
Blakey 105Ma - COL.jpg
Paleogeography of Northern South America
105 Ma, by Ron Blakey

The Pacho Formation (Spanish: Limolitas de Pacho, Kslp) is a geological formation of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consisting of alternating siltstones and shales with siderite concretions dates to the Middle Cretaceous period; Late Albian to Cenomanian epochs and has an approximate thickness of 1,050 metres (3,440 ft).

Etymology

The formation was defined and named in 1982 by Ulloa after Pacho, Cundinamarca.[1]

Description

Lithologies

The Pacho Formation has an approximate thickness of 1,050 metres (3,440 ft), and is characterised by a sequence of alternating siltstones and shales with siderite concretions.[1]

Stratigraphy and depositional environment

The Pacho Formation, pertaining to the Villeta Group, partly overlies and is partly lateral equivalent with the Hiló Formation and is partly overlain by and partly time equivalent with the Simijaca Formation. The age has been estimated to be Late Albian to Cenomanian. Stratigraphically, the formation is time equivalent with the Une Formation. The formation has been deposited in an outer marine platform environment.[1]

Outcrops

Lua error in Module:Location_map at line 522: Unable to find the specified location map definition: "Module:Location map/data/Bogotá savanna" does not exist. The Pacho Formation is found around its type locality near Pacho.[1]

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 1.3 Acosta & Ulloa, 2002, p.45

Bibliography

Maps

External links