ArticleACS omega2026
The Origin of Middle Triassic Thick Anhydrite in the Lower Yangtze Region, South China: Implications for the Evolution of Lithium-Rich Brine.
Article in ACS omega, 2026. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.
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Abstract
Lithium-(Li)-rich brines represent an increasingly important strategic resource and are commonly associated with evaporites. Their formation has traditionally been mainly attributed to evaporation-driven concentration under arid paleoclimatic conditions. This study investigates the genetic mechanism of the thick anhydrite deposits and associated lithium-rich brines in the Middle Triassic Zhouchongcun Formation of the Lower Yangtze region. Through integrating petrographic, elemental, and isotopic geochemistry and fluid inclusion analyses, combined with reconstruction of the stratigraphic burial-thermal history, we demonstrate that the formation and evolution of these evaporates are closely linked to multiple tectonic-thermal events. Petrographic characteristics and carbon-oxygen isotopic data indicate that the anhydrite initially formed in a restricted evaporative environment during the Middle Triassic, with δ
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