= Ulrich H. Faul
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<Ulrich H. Faul> coauthored lunar models using a laboratory-calibrated description of <anelasticity> in melt-free <olivine>. This connects small-scale mineral deformation with measurable planetary energy loss.<Dissipation at tidal and seismic frequencies in a melt-free Moon by Francis Nimmo and others>[Abstract: deformation-based rheological model]{ref}
Such a comparison tests whether solid-state relaxation can explain observations before an additional molten layer is required.
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