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The centre-of-mass–centre-of-figure (COM–COF) offset of Mars also limits the potential compositional component (for example, iron, water content) of asymmetries because, in isolation, such differences (and their associated density structure) would need to produce an offset that is approximately 50 times larger
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https://www.nature.com/articles/s41586-026-10893-x
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https://www.nature.com/articles/s41467-026-76671-5
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https://www.nature.com/articles/s41586-026-11035-z
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https://www.nature.com/articles/s41586-026-10900-1
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https://www.nature.com/articles/s44271-026-00473-0
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https://www.nature.com/articles/s41586-026-10916-7
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https://www.nature.com/articles/s41586-026-10876-y
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https://www.nature.com/articles/s41586-026-11034-0
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https://www.nature.com/articles/s41586-026-11024-2
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https://www.nature.com/articles/ngeo2580
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https://www.nature.com/articles/s41586-026-10979-6
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https://www.nature.com/articles/s41586-026-11026-0
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https://www.nature.com/articles/s41586-026-11032-2
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https://www.nature.com/articles/s41561-026-02070-6
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https://www.nature.com/articles/s41594-022-00857-w
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https://www.nature.com/articles/s41586-026-10905-w
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https://www.nature.com/articles/s41586-026-10907-8
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https://www.nature.com/articles/s43247-026-03242-3
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https://www.nature.com/articles/s41597-024-04135-w
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https://www.nature.com/articles/nature12774
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