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

Komatii Formation

From Wikipedia, the free encyclopedia

Komati Formation
Stratigraphic range: Paleoarchean
TypeGeological formation
Unit ofOnverwacht Group
 Tjakastad Subgroup
UnderliesGeluk Subgroup
 Hooggenoeg Formation
OverliesTheespruit Formation
Thickness3,500 m (11,500 ft)
Lithology
PrimaryKomatiite
OtherTholeiite
Location
Coordinates25°48′S 31°00′E / 25.8°S 31.0°E / -25.8; 31.0
RegionBarberton Greenstone Belt, Mpumalanga
Country South Africa
ExtentKaapvaal Craton
Type section
Named forKomati River

Location of the Barberton Greenstone Belt

The Komati Formation, also named as Komatii Formation, is a 3.475 billion year old Paleoarchean rock formation, named after the nearby Komati River in South Africa. It is the type locality for komatiite, a high temperature, magnesium-rich volcanic rock occurring in the Barberton Greenstone Belt, Mpumalanga.[1]

Description

The formation, belonging to the Tjakastad Subgroup of the Onverwacht Group, overlies the Theespruit Formation and is overlain by the Hooggenoeg Formation of the Geluk Subgroup.[2] Komatiites and tholeiites from the Komati Formation were analyzed for sulfur and provided δ34S values between −0.7 and 5.2 ‰.[3]

The Komatii Formation comprises metamorphosed komatiites and basaltic komatiites, with minor mafic lavas and small intrusions. The lower part of the Komatii Formation is dominantly ultramafic, while the upper part is dominantly mafic.[4]

References

  1. ^ Greenstone Belt Studies, Department of Geological Sciences, University of Cape Town
  2. ^ Montinaro et al., 2015, p.314
  3. ^ Montinaro et al., 2015, p.319
  4. ^ Guice, 2019, p.143

Bibliography

  • Guice, George L (2019). Origin and geodynamic significance of ultramafic-mafic complexes in the North Atlantic and Kaapvaal Cratons (PhD thesis). Cardiff University. pp. 1–289.
  • Montinaro, Alice; Strauss, Harald; Mason, Paul R.D.; Roerdink, Desiree; Münker, Carsten; Schwarz-Schamper, Ulrich; Arndt, Nicholas T.; Farquhar, James; Beukes, Jens Gutzmer and Marc Peters, Nicolas J. (2015). "Paleoarchean sulfur cycling: Multiple sulfur isotope constraints from the Barberton Greenstone Belt, South Africa". Precambrian Research. 267: 311–322.
This page was last edited on 18 June 2023, at 19:55
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.