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Tidal evolution of Earth-like planets in the habitable zone of low-mass stars
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Earth-Moon dynamics from cyclostratigraphy reveals possible ocean tide resonance in the Mesoproterozoic era
Maoyang Zhou, Huaichun Wu, Linda A. Hinnov, Qiang Fang, Shihong Zhang, Tianshui Yang and Meinan Shi Science Advances 10(31) (2024) https://doi.org/10.1126/sciadv.adn7674
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Mass–Radius Relationships and Contraction of Condensed Planets by Cooling or Despinning
Astronomical timescale across the middle Permian–Early Triassic unconformities in the northwestern Junggar Basin: Implications for the origin of the unconformities
Exomoons and Exorings with the Habitable Worlds Observatory. I. On the Detection of Earth–Moon Analog Shadows and Eclipses
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Kepler-discovered Multiple-planet Systems near Period Ratios Suggestive of Mean-motion Resonances Are Young
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Anthony Lagain, Hadrien A.R. Devillepoix, Pierre Vernazza, Darrel Robertson, Mikael Granvik, Petr Pokorny, Anthony Ozerov, Patrick M. Shober, Laurent Jorda, Konstantinos Servis, John H. Fairweather, Yoann Quesnel and Gretchen K. Benedix Icarus 411 115956 (2024) https://doi.org/10.1016/j.icarus.2024.115956
The Faustini Permanently Shadowed Region on the Moon
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Rapid solidification of Earth’s magma ocean limits early lunar recession
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Oblique rings from migrating exomoons: A possible origin for long-period exoplanets with enlarged radii
North Atlantic Drift Sediments Constrain Eocene Tidal Dissipation and the Evolution of the Earth‐Moon System
David De Vleeschouwer, Donald E. Penman, Simon D'haenens, Fei Wu, Thomas Westerhold, Maximilian Vahlenkamp, Carlotta Cappelli, Claudia Agnini, Wendy E. C. Kordesch, Daniel J. King, Robin van der Ploeg, Heiko Pälike, Sandra Kirtland Turner, Paul Wilson, Richard D. Norris, James C. Zachos, Steven M. Bohaty and Pincelli M. Hull Paleoceanography and Paleoclimatology 38(2) (2023) https://doi.org/10.1029/2022PA004555
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Earth's rotation and Earth-Moon distance in the Devonian derived from multiple geological records
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Milankovitch cycles in banded iron formations constrain the Earth–Moon system 2.46 billion years ago
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