Sentinel Vision - Story EVT-243

Fig. 1 - Sentinel-2 (14.09.2017) - 11,8,2 colour composite, relief x10 - View of the Richat structure in Mauritania.

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Pr. Jean Chorowicz, emeritus Professor of University Paris 6 wrote: "The spectacular Richat circular structure (Mauritania) – famous ‘Eye of the Sahara’ - appears as alternating types of rocks forming concentric rings. It lies down a circular scarp and shows a Late Proterozoic to Early Palaeozoic rock sequence. Inside, erosion has created circular cuestas dipping outward from the structure. By places, can also be identified a volcanic crater (with a sebkhra inside), a kimberlitic plug, light coloured carbonatite dykes (more frequent in southern part of the structure), rhyolitic volcanites, high-K gabbroic ring dykes."

Fig. 2 - Sentinel-1 (24.11.2017) - vv,vh,vv colour composite - Dry sandy areas appears in dark, reliefs facing the radar beam in bright

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He describes the geological context, writing "the structure lies in the Reguibat Shield, northern part of the West African Craton. Further to the west (Geological Map of Africa, CGMW) there is a succession of stacked nappes of Variscan age (late Palaeozoic), part of the Mauritanides-Appalaches orogen lying now along both sides of the Atlantic for it served at around 100 Ma as the major lithospheric discontinuity reactivated by evolution of a proto-Atlantic continental rift and opening of the Atlantic Ocean."

Fig. 3 - SRAL - Height computed from "ocean" altimeter range 20hz Ku over a S1 vv,vh,ndi(vh,vv) composite - Topographic variations of Richat

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Fig. 4 - SRAL - Peakiness 20Hz: Ku band (rainbow), Plrm Ku band (pink line) & C band (black line) - Peakiness over Richat's complex structure.

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Fig. 5 - S2 - Zoom on carbonatite dykes in the ring layers.

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Regarding carbonatites, he adds: "The center consists of a limestone-dolomite shelf that encloses siliceous breccia created during karst dissolution and collapse. Carbonatites are sub-surface intrusive magmatic rocks, essentially crystalline limestone or dolomite, originating from deep magma enriched in Ca and CO2. They have the highest rare earth element (REE) concentrations of all igneous rocks. Age of the intrusion is ~100 Ma (middle of the Cretaceous). There are ring faults and numerous small straight faults."

Fig. 6 - S1 - The volcanic crater (encased), partly in the radar shadow, appears darker than nearby mega-breccias of limestone & dolomite.

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Professor Jean Chorowicz finally describes: "The evolution of the structure is thought to be as follows

Ancient subduction-collision process may have favored the assimilation in the continental lithosphere of preexisting subducted sedimentary carbonates, forming a carbonatite melt. Another debated hypothesis is that carbonatite and proto-kimberlite magmas are related to mantle plume activity, which had played a part in the proto-Atlantic rift evolution.

Mid-Cretaceous breakup of Gondwana continent may have provided opportunities for this magma to reach the sub-surface.

Intrusions induced the uplift of a dome at the surface with, beneath, accumulation of a mushroom-like carbonatite body, fed by dykes and ring dykes.

Subsequent erosion and thermal activity dissolved most of the carbonatite, from which remained karstic breccia and the root of the structure.”

Fig. 7 - S2 - Zoom showing gabbro ring dykes encased in green, note the white sebkha in the crater.

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Fig. 8 - S2 - Zoom on a kimberlitic plug in an outer ring.

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The views expressed herein can in no way be taken to reflect the official opinion of the European Space Agency or the European Union.
Contains modified Copernicus Sentinel data 2024, processed by VisioTerra.

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