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Video Credit: Southwest Research Institute |
Southwest Research Institute’s Dr. Simone Marchi collaborated on a new study finding the first geophysically plausible scenario to explain the abundance of certain precious metals — including gold and platinum — in the Earth’s mantle. Based on the simulations, or model, scientists found that impact-driven mixing of mantle materials scenario that could prevent the metals from completely sinking into the Earth’s core.
Early in its evolution, about 4.5 billion years ago, Earth sustained an impact with a Mars-sized planet, and the Moon formed from the resulting debris ejected into an Earth-orbiting disk. A long period of bombardment followed, the so-called “late accretion,” when planetesimals as large as our Moon impacted the Earth delivering materials including highly “siderophile” elements (HSEs) — metals with a strong affinity for iron — that were integrated into the young Earth.
“Previous simulations of impacts penetrating Earth’s mantle showed that only small fractions of a metallic core of planetesimals are available to be assimilated by Earth’s mantle, while most of these metals — including HSEs — quickly drain down to the Earth’s core,” said Marchi, who coauthored a Proceedings of the National Academy of Sciences (PNAS) paper outlining the new findings. “This brings us to the question: How did Earth get some of its precious metals? We developed new simulations to try to explain the metal and rock mix of materials in the present-day mantle.”