3. Concentrating natural phenomena, deposits, reserves and production
3.1 Magnesium concentrator phenomena
They are at the origin of sedimentary-type deposits resulting from the evaporation of seawater. The genesis of evaporites is complex, as a result of reworking, flooding, meteorological variations, leaching by rainwater or the decomposition of double salts, such as carnalite, which decomposes into sylvinite. However, the evaporitic series can be considered, from bottom to top, as the following sedimentary sequence:
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Concentrating natural phenomena, deposits, reserves and production
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