Tectonic development of the northern Taiizaiiian sector of the East African Rift System

@article{Foster1997TectonicDO,
  title={Tectonic development of the northern Taiizaiiian sector of the East African Rift System},
  author={A. Foster and Cynthia J. Ebinger and Evelyne Mbede and David C. Rex},
  journal={Journal of the Geological Society},
  year={1997},
  volume={154},
  pages={689 - 700}
}
The Eastern Branch of the East African Rift System diverges from a single, c. 50 km wide rift in southern Kenya to a c. 200 km wide zone in northern Tanzania, where it is comprised of three distinct rifts with different orientations. The western part of this zone contains two rift branches: the Natron-Man yara-Balangida and Eyasi-Wembere rifts. Each rift contains individual basins that are defined here on the basis of structural and geophysical interpretations. These basins are shallow (<3km… 

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