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- Geodynamics_of_Mars abstract "Mars was a geologically active place during its first billion years of existence, and particularly during its first 50 million years or so. In this time a metallic core, silicate mantle, and more than half of the crust formed by major melting. Within 15 million years (Ma) of the start of the solar system, a metallic core was made by iron dribbling to the center of the planet.Both short-lived and long-lived radiogenic isotopes indicate that a large-ion lithophile enriched reservoir (which is the early "crustal" reservoir) separated from the primitive mantle very early in the history of Mars. Exact timing is less clear and generally model dependent but an age certainly in excess of 4.0 Ga and possibly approaching 4.5 Ga is likely.".
- Geodynamics_of_Mars thumbnail Mars_Hubble.jpg?width=300.
- Geodynamics_of_Mars wikiPageID "42344134".
- Geodynamics_of_Mars wikiPageRevisionID "606262907".
- Geodynamics_of_Mars subject Category:Surface_features_of_Mars.
- Geodynamics_of_Mars comment "Mars was a geologically active place during its first billion years of existence, and particularly during its first 50 million years or so. In this time a metallic core, silicate mantle, and more than half of the crust formed by major melting.".
- Geodynamics_of_Mars label "Geodynamics of Mars".
- Geodynamics_of_Mars sameAs m.010ff9wy.
- Geodynamics_of_Mars sameAs Q17076696.
- Geodynamics_of_Mars sameAs Q17076696.
- Geodynamics_of_Mars wasDerivedFrom Geodynamics_of_Mars?oldid=606262907.
- Geodynamics_of_Mars depiction Mars_Hubble.jpg.
- Geodynamics_of_Mars isPrimaryTopicOf Geodynamics_of_Mars.
