Stable Brine Layers beneath Europa’s Chaos

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Abstract

The formation mechanism of Europa’s large chaos terrain (>∼100 km diameter) and associated lenticulae (

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Chivers, C. J., Buffo, J. J., & Schmidt, B. E. (2023). Stable Brine Layers beneath Europa’s Chaos. Planetary Science Journal, 4(9). https://doi.org/10.3847/PSJ/acea75

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