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The Reocin deposit, which displays no visible relationship with a magmatic source, is located in the upper, dolomite-rich part of the Aptian series and more precisely in the lower 40 m of the dolomite-rich rocks. Sedimentology and mineralography, as well as other approaches are used to define the environment of deposition.

In short, the following generalizations hold: the only mineralized rocks are the Upper Aptian dolostones; the mineralization is stratigraphically controlled; where the dolostones become thinner and pinch out, so do the ore beds. But not all dolostones are mineralized. The three ore beds found in the Central Area...

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