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1. Reactive eclogitization

   https://doi.org/10.5281/zenodo.14805160  

   McMillan, Mitchell (February 2025, Zenodo)

   Official repository: https://gitlab.com/mitchellmcm27/eclogite-tcg 

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2. Estimating benthic Fe and reactive solute fluxes

   https://doi.org/10.1016/j.marchem.2023.104221  

   Aller, R.C.; Dwyer, I.P.; Perger, D.A. Swenson; Heilbrun, C.; Volkenborn, N.; Wehrmann, L.M. (February 2023, Marine Chemistry)
3. Reactive thermodynamics of crustal eclogitization and foundering

   McMillan, Mitchell; Sim, Shi J; Wilson, Cian R (May 2025, Earth and planetary science letters)

   Regional metamorphism and densification (eclogitization) of the lower crust can affect the lithospheric dynamics of mountain belts, but the coupled effects of reaction rate, temperature, and composition on metamorphism are poorly understood. We present a reactive thermodynamic model of the granulite–eclogite transition to investigate the long-term buoyancy and gravitational stability of the lower crust. First, we characterize the conditions for which orogenic crust attains negative buoyancy by determining its reactive mineral assemblage and density under prescribed pressure–temperature–time paths. Using existing metamorphic rate data, we calibrate a Damkoḧler number (a relative reaction rate) to parameterize the catalytic effect of aqueous fluids. The depth necessary for negative buoyancy is sensitive to temperature and Da, ranging from ∼45 to Image 1 for a basaltic-andesite composition (54 wt.% SiO2). Second, using a Rayleigh–Taylor instability analysis, we suggest that, while cold eclogitic crusts Image 2 could obtain large thicknesses of ∼10 to Image 3 and would founder within Image 4. We hypothesize that such foundering events are a natural consequence of convergent tectonics, where the aqueous fluids and high pressures required for metamorphism are known to exist. The Pampean flat slab in the Central Andes provides geophysical evidence linking slab fluids to eclogitization and densification of the thickened continental crust. Lithospheric foundering coupled to convergent tectonics through eclogitization could explain many observations of orogenic hinterland deformation and magmatism. 

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4. Sulfate production by reactive bromine: Implications for the global sulfur and reactive bromine budgets: Sulfur-Halogen Interactions

   https://doi.org/10.1002/2017GL073812  

   Chen, Q.; Schmidt, J. A.; Shah, V.; Jaeglé, L.; Sherwen, T.; Alexander, B. (July 2017, Geophysical Research Letters)
5. Mantis: Reactive Programmable Switches

   https://doi.org/10.1145/3387514.3405870  

   Yu, Liangcheng; Sonchack, John; Liu, Vincent (July 2020, Proceedings of the Annual conference of the ACM Special Interest Group on Data Communication on the applications, technologies, architectures, and protocols for computer communication)

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