Tuareg shield

The Tuareg Shield is an area lying between the West African craton and the Saharan Metacraton in West Africa. Named after the Tuareg people, it has complex a geology, reflecting the collision between these cratons and later events. The landmass covers parts of Algeria, Niger and Mali.

The Tuareg Shield is mainly composed of Archean or Paleoproterozoic terranes and Neoproterozoic terranes that amalgamated during the Pan African orogeny when the West African craton and the Saharan metacraton converged.

The shield originated in oceanic island arcs that formed on the cratons during 900 Ma to 680 Ma, of which relics remain as thrust sheets on top of more rigid bodies.

In Mali, the Tilemsi belt is a complex of intraoceanic arcs that formed above a subduction zone sloping down to the east and were accreted to the shield during the Pan-African orogeny.

The western part of the Hoggar massif (Ahaggar Mountains) is made of material from the Pharusian Ocean including oceanic basalts, arc volcanic and sedimentary rocks and sediments that were shed into the Pharusian Ocean by the West African craton and the eastern Hoggar.

During the oblique collision of the West African craton with the Saharan metacraton, the shield was torn into separate but rigid moving blocks. These blocks were separated by subvertical shear zones.

The fractured shield was penetrated by volcanic magmas that formed the Hoggar in Algeria, Adrar des Iforas in Mali and Aïr Mountains in Niger.

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