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Lithium replenishment in geothermal extraction operations occurs primarily through release from phyllosilicates such as chlorite, illite, and biotite, a process that is significantly enhanced by hypersaline solutions but largely independent of temperature between 100 and 160 °C. Novelty: ClaimNovelty.NOVEL_FINDING. Consensus alignment: ConsensusAlignment.NEUTRAL.

Hydrothermal experiments at in-situ conditions to identify Li release reactions by water-mineral interactions in deep sedimentary basins of the North German Basin and Upper Rhine Graben

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