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The "eye of Africa" (Richat dome, Mauritania): An isolated Cretaceous alkaline–hydrothermal complex

Guillaume Matton, Michel Jébrak, 2014. Journal of African Earth Sciences 97: 109-124.

Petrological and structural synthesis of the Richat complex: a bimodal tholeiitic suite cut by carbonatite and kimberlite, a low-temperature hydrothermal event that made the central karst-collapse breccia, and a piston-like collapse of the centre.

MYS0DCKKMWKKKPC · mystery · click to copyMEye of the Sahara and AtlantisSecondary sourceArticledoi: 10.1016/j.jafrearsci.2014.04.006Checked against the original0

What it's used for here

Cited for the full igneous suite (gabbro ring dikes, rhyolite maars, carbonatite, kimberlite), the hydrothermal event, the 20–30 m relief of the ridges and the inferred 104–94 Ma age of the complex.

Cited by on this site 4 records

Cite it

Matton, G., & Jébrak, M. (2014). The "eye of Africa" (Richat dome, Mauritania): An isolated Cretaceous alkaline–hydrothermal complex. Journal of African Earth Sciences, 97, 109-124. https://doi.org/10.1016/j.jafrearsci.2014.04.006
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