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Cited article:

Titan’s refractory core evolution: Implications for organics in its subsurface ocean

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Experimental heating of complex organic matter at Titan’s interior conditions supports contributions to atmospheric N2 and CH4

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The formation of cone chains in the Chryse Planitia region on Mars and the thermodynamic aspects of this process

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Laboratory exploration of mineral precipitates from Europa's subsurface ocean

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Self-preserving ice layers on CO2 clathrate particles: Implications for Enceladus, Pluto, and similar ocean worlds

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Do Oceanic Convection and Clathrate Dissociation Drive Europa’s Geysers?

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The Planetary Science Journal 2 (6) 221 (2021)
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Electrochemical Conversion of CO2 and CH4 at Subzero Temperatures

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Structure and Physicochemical Properties of Water Treated under Carbon Dioxide with Low-Temperature Low-Pressure Glow Plasma of Low Frequency

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X-ray powder diffraction study of the stability of clathrate hydrates in the presence of salts with relevance to the Martian cryosphere

Emmal Safi, Stephen P. Thompson, Aneurin Evans, Sarah J. Day, Claire A. Murray, Annabelle R. Baker, Joana M. Oliveira and Jacco Th. van Loon
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Dispersion Forces Stabilize Ice Coatings at Certain Gas Hydrate Interfaces That Prevent Water Wetting

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Insights into Ceres's evolution from surface composition

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Meteoritics & Planetary Science 53 (9) 1820 (2018)
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