To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
Languages
Recent
Show all languages
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

Cheuquemó Formation

From Wikipedia, the free encyclopedia

Cheuquemó Formation
Stratigraphic range: Late OligoceneEarly Miocene
Unit ofOsorno–Llanquihue Basin
UnderliesSanto Domingo Formation
OverliesBahía Mansa Metamorphic Complex
Thicknessmore than 1,200 m (3,900 ft)
Lithology
PrimaryConglomerate, sandstone, mudstone, tuff
OtherCoal
Location
Coordinates40°00′S 73°00′W / 40.0°S 73.0°W / -40.0; -73.0
RegionLos Lagos Region
Country Chile
Type section
Named byFloreal García
Year defined1968
Cheuquemó Formation (Chile)

Cheuquemó Formation (Spanish: Formación Cheuquemó) is a geological formation of sedimentary rock in south-central Chile. The sediments of the formation were deposited during the Late Oligocene and Early Miocene epochs. The formations lower sections are made up of conglomerate, then successions of sandstone, tuff and mudstone rich in organic material follows. The formation indicates that sedimentation occurred in an estuarine (paralic) and other non-marine (continental) environments. It contains fossils of the following genera: Mytilus, Cardium and Turritella. Stratigraphically it overlies the Bahía Mansa Metamorphic Complex and underlies the Miocene Santo Domingo Formation.[1]

Description

The formation is very similar to the Pupunahue Beds found further north, with the sole difference that the fossil assemblage in both seem to indicate different ages. While Cheuquemó is possibly about 14 million years old (Miocene), the Pupunahue Beds are 35–25 million years old.[2]

See also

References

  1. ^ Elgueta, Sara; Le Roux, Jacobus; Duhart, Paul; McDonough, Michael; Urqueta, Esteban (2000). Estratigrafía y sedimentología de la cuencas terciarias de la Región de Los Lagos (39-41°30'S) (in Spanish). Santiago, Chile: Servicio Nacional de Geología y Minería. pp. 15–16. ISSN 0020-3939.
  2. ^ Alfaro, G.; Gantz, E.; Magna, O. (1990). "El yacimiento de carbón Catamutún (La Unión)". Actas. Segundo Simposio sobre el Terciario de Chile (in Spanish). Santiago, Chile: Departamento de Geociencias, Facultad de Ciencias, Universidad de Concepción. pp. 11–28.
This page was last edited on 12 June 2024, at 12:53
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.