๐งญ๐ฆ Hydrogeochemical & Isotopic ๐ Clues to ๐ Deep Hypersaline Brine Formation via Radiolysis!
๐งช๐ This study investigates deep subsurface hypersaline brines using hydrogeochemical patterns and isotopic fingerprints.
⚡๐ชจ Findings show that radiolysis-driven water–rock interactions play a key role in generating and evolving these ancient saline fluids.
๐ง๐ฌ The results enhance understanding of hidden geochemical processes and the long-term ๐งญdynamics of Earth’s deep hydrological systems. ๐๐ก
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