Structural Geology of the Afar
Region
The movements of the Nubian, Arabian and Somalian plates over the past
30 million years or so have created a series of different tectonic regimes
across the Afar region each with their own distinct structural style (e.g.
Hayward & Ebinger, 1996; Hofstetter & Beyth, 2003; Beyene &
Abdelsalam, 2005). These are:
The Afar Depression
Northern Afar Rift
Dabbahu Magmatic
Segment
East-Central Afar Rift
Southern Afar Rift
Ethiopian and Somalian plateaux
Danakil and Ali-Sabieh Blocks
Southern Red Sea and Gulf of Aden
Main Ethiopian Rift (MER)
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