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  2. Barberton Greenstone Belt - Wikipedia

    en.wikipedia.org/wiki/Barberton_Greenstone_Belt

    The Barberton Mountain is a well preserved pre-3.0 Ga granite-greenstone terrane. The greenstone belt consists of a sequence of mafic to ultramafic lavas and metasedimentary rocks emplaced and deposited between 3.5 and 3.2 Ga. The granitoid rocks were emplaced over a 500 million year time span and can be divided into two suites.

  3. File:Simplified geologic map of the Barberton greenstone belt.pdf

    en.wikipedia.org/wiki/File:Simplified_geologic...

    Description Simplified geologic map of the Barberton greenstone belt.pdf. English: This is a simplified geologic map of the Barberton Greenstone belt, South Africa, showing three of the major Groups and their interactions as well as the Kaap Valley Craton. Date. 10 October 2013, 15:38:59. Source.

  4. Archean life in the Barberton Greenstone Belt - Wikipedia

    en.wikipedia.org/wiki/Archean_life_in_the...

    The Barberton Greenstone Belt of eastern South Africa contains some of the most widely accepted fossil evidence for Archean life. These cell -sized prokaryote fossils are seen in the Barberton fossil record in rocks as old as 3.5 billion years. [1] The Barberton Greenstone Belt is an excellent place to study the Archean Earth due to exposed ...

  5. Greenstone belt - Wikipedia

    en.wikipedia.org/wiki/Greenstone_belt

    Kilimafedha greenstone belt in Tanzania. Greenstone belts are zones of variably metamorphosed mafic to ultramafic volcanic sequences with associated sedimentary rocks that occur within Archaean and Proterozoic cratons between granite and gneiss bodies. The name comes from the green hue imparted by the colour of the metamorphic minerals within ...

  6. Makhonjwa Mountains - Wikipedia

    en.wikipedia.org/wiki/Makhonjwa_Mountains

    The Makhonjwa Mountains or Barberton Makhonjwa Mountains are a range of small mountains and hills that covers an area of 120 by 60 kilometres (75 by 37 mi), about 80% in Mpumalanga, a province of South Africa, and the remainder in neighbouring Eswatini. [2] It constitutes 40% of the Barberton Greenstone Belt. [3]

  7. Kaapvaal Craton - Wikipedia

    en.wikipedia.org/wiki/Kaapvaal_Craton

    The craton is a mixture of early Archean (3.0–3.5 Ga) granite greenstone terranes and older tonalitic gneisses (ca. 3.6–3.7 Ga), intruded by a variety of granitic plutons (3.3–3.0 Ga). Subsequent evolution of the Kaapvaal Craton (3.0–2.7 Ga) is thought to be associated with continent–arc collision that caused an overlaying succession ...

  8. Tectonic evolution of the Barberton greenstone belt - Wikipedia

    en.wikipedia.org/wiki/Tectonic_evolution_of_the...

    The Barberton greenstone belt (BGB) is located in the Kapvaal craton of southeastern Africa. It characterizes one of the most well-preserved and oldest pieces of continental crust today by containing rocks in the Barberton Granite Greenstone Terrain (3.55–3.22 Ga ). The BGB is a small, cusp-shaped succession of volcanic and sedimentary rocks ...

  9. Barberton, South Africa - Wikipedia

    en.wikipedia.org/wiki/Barberton,_South_Africa

    Barberton is a town in the Mpumalanga province of South Africa, which has its origin in the 1880s gold rush in the region. It is situated in the De Kaap Valley and is fringed by the Makhonjwa Mountains. It is 43 kilometres (27 mi) south of Mbombela and 360 kilometres (220 mi) east of Johannesburg . Barberton was the seat of the Umjindi Local ...