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Sebakwian Group

geological feature, Africa

Quick Summary

The Sebakwian Group refers to geological formations found in Zimbabwe, Africa, dating back approximately 3.8 to 3.75 billion years ago. These formations are part of the larger greenstone-granite belts, which are considered ancient slices of oceanic and island arc crust that have been tectonically assembled.1

These belts are characterized by volcanic rocks, including ultramafic and basaltic lavas, and overlying sedimentary layers such as shales and sandstones. The term "greenstone" comes from the metamorphic minerals like chlorite and epidote that form during low-temperature and low-pressure metamorphism. The Sebakwian Group represents an early stage in the Earth's crustal evolution during the Archean Eon.12

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