The Tanzania Craton is an old and stable part of the continental lithosphere in central Tanzania. Some of the rocks are over 3 billion years old.[1]
Setting
The Tanzania Craton forms the highest part of the East African Plateau.[2] The craton is surrounded by Proterozoic mobile belts of various ages and grades of metamorphism. These include the Ubendian, Usagaran, Karagwe-Ankolean and Bukoban systems. The Mozambique Belt lies to the east.[3] The craton divides the east and west branches of the East African Rift.[2] The southern end of the Gregory Rift Valley terminates against the craton. The volcanic area of this rift covers the surface interface between the Mozambique orogenic fold belt and the Tanzania Craton.[1] A superplume exists beneath the craton.[4][5] An indirect effect of rift and plume associated volcanism in the Tanzania Craton is the high levels of soil nutrients in Serengeti provided by volcanic ash from Ol Doinyo Lengai.[6]
Composition
The craton is a composite of several different terranes of Archaean metasediments. The Dodoman is the oldest, and others include the Nyanzian and Kavirondian. Some of the greenstone belts are more than 3 billion years old. They were intruded by granites and migmatized in different events that date back to 2.9, 2.7, 2.4 and 1.85 billion years ago.[1] The craton mainly consists of Archaean granitic complexes, but also includes rocks from the Dodoma System in the central area, and belts of greenstone to the south and east of Lake Victoria. Gneisses, schists, quartzites, migmatites, amphibolites and granulite are also found. There was widespread intrusion of kimberlites in the Cretaceous Period, mostly in the part of the craton that lies south of Lake Victoria.[3] This includes the Mwadui kimberlite pipe in the center of Tanzania.[7]
References
- ^ a b c Dawson 2008, p. 9.
- ^ a b Dawson 2008, p. 2.
- ^ a b Geological Framework.
- ^ Mulibo, Gabriel D.; Nyblade, Andrew A. (28 July 2013). "Mantle transition zone thinning beneath eastern Africa: Evidence for a whole-mantle superplume structure". Geophysical Research Letters. 40 (14): 3562–3566. Bibcode:2013GeoRL..40.3562M. doi:10.1002/grl.50694. S2CID 53640435.
- ^ Figure 13 in Hui, Hejiu; Peslier, Anne H.; Rudnick, Roberta L.; Simonetti, Antonio; Neal, Clive R. (April 2015). "Plume‐cratonic lithosphere interaction recorded by water and other trace elements in peridotite xenoliths from the Labait volcano, Tanzania". Geochemistry, Geophysics, Geosystems. 16 (6): 1687–1710. Bibcode:2015GGG....16.1687H. doi:10.1002/2015GC005779. S2CID 37882729. Retrieved 4 August 2017.
- ^ "The Strangest Volcanoes In The World – A Non-Official List". 28 March 2017. Retrieved 4 August 2017.
- ^ van Straaten 2009, p. 280.
Sources
- Dawson, John Barry (2008). The Gregory rift valley and Neogene-recent volcanoes of northern Tanzania. Geological Society. ISBN 978-1-86239-267-0.
- "GEOLOGICAL FRAMEWORK AND REGIONAL METALLOGENY OF TANZANIA" (PDF). Kilimanjaro Mining Company. Retrieved 2011-12-28.
- van Straaten, Peter (2009). "Tanzania" (PDF). Rocks for Crops. University of Guelph.
This page was last edited on 20 November 2023, at 02:49