The Contraction/Expansion History of Charon with implication for its Planetary Scale Tectonic Belt
Uri Malamud, Hagai B. Perets, Gerald Schubert

TL;DR
This study uses a detailed thermo-physical evolution model to explain Charon's surface tectonic features as resulting from contraction and expansion episodes, without requiring a subsurface ocean or warm initial state.
Contribution
It introduces a new model of Charon's evolution that accounts for tectonic belt formation through internal contraction/expansion episodes, challenging previous ocean-based hypotheses.
Findings
Charon experienced two major contraction/expansion episodes.
The tectonic belt likely formed during these episodes, not from a subsurface ocean.
A planetary-scale impact may have shaped the observed features.
Abstract
The New Horizons mission to the Kuiper Belt has recently revealed intriguing features on the surface of Charon, including a network of chasmata, cutting across or around a series of high topography features, conjoining to form a belt. It is proposed that this tectonic belt is a consequence of contraction/expansion episodes in the moon's evolution associated particularly with compaction, differentiation and geochemical reactions of the interior. The proposed scenario involves no need for solidification of a vast subsurface ocean and/or a warm initial state. This scenario is based on a new, detailed thermo-physical evolution model of Charon that includes multiple processes. According to the model, Charon experiences two contraction/expansion episodes in its history that may provide the proper environment for the formation of the tectonic belt. This outcome remains qualitatively the same,…
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