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Abstract: Evolution of subaerial cratonic exposure through the lens of low-δ¹⁸O meteoric hydrothermal systems: An update on an intact Neoarchean system from Kola Craton based on multiple isotope proxies (H, Si, triple O, Hf) (AGU25)

Evolution of subaerial cratonic exposure through the lens of low-δ¹⁸O meteoric hydrothermal systems: An update on an intact Neoarchean system from Kola Craton based on multiple isotope proxies (H, Si, triple O, Hf)

David O Zakharov, Western Michigan University, Kalamazoo, United States, Dmitry Zozulya, Geological Institute, Kola Science Centre of the Russian Academy of Sciences, Apatity, Russia, Massimo Chiaradia, University of Geneva, Geneva, Switzerland, Patrick Frings, Deutsches GeoForschungsZentrum GFZ, Potsdam, Germany and Anne-Sophie Bouvier, University of Lausanne, Institute of Earth Sciences, Lausanne, Switzerland
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