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posted by martyb on Friday October 06 2017, @06:42AM   Printer-friendly
from the prepare-for-a-coverup dept.

Scientists have long assumed that all the planets in our solar system look the same beneath the surface, but a study published in Geology on Oct. 4 tells a different story.

"The mantle of the earth is made mostly of a mineral called olivine, and the assumption is usually that all planets are like the Earth," said Jay Melosh, a professor of earth, atmospheric and planetary sciences at Purdue University, who led the study. "But when we look at the spectral signature of rocks exposed deep below the moon's surface, we don't see olivine; we see orthopyroxene."

Around 4 billion years ago, an asteroid collided with the moon and created the largest and deepest impact on the moon: the South Pole-Aitken basin. The collision exposed lunar mantle in the basin and splashed up material onto the far side of the moon.

Melosh's group used remote sensing to identify what minerals compose the splashed-up material. When sunlight hits the moon, it interacts with materials on the surface; because different materials absorb different wavelengths of light, researchers can tell what materials are on the surface by looking at the reflected signal.

Wallace and Gromit will be disappointed to learn it's not Stilton.

South Pole‚ÄďAitken basin ejecta reveal the Moon's upper mantle (DOI: 10.1130/G39375.1) (DX)


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  • (Score: 2) by Taibhsear on Friday October 06 2017, @08:18PM

    by Taibhsear (1464) on Friday October 06 2017, @08:18PM (#578310)

    Could be a variation on that theory. In the link I posted it says around 10-40% of the moon's mass is from Pre-Earth and the rest is from Theia.
    This link explains further. The collision basically disintegrated/vaporized/liquified Theia and ejected it. It then coalesced/formed into the moon. There's competing theories for what happened after that because one side of the moon has a thicker crust.
    http://www.slate.com/blogs/bad_astronomy/2014/07/01/the_moon_s_two_faces_why_are_they_so_different.html [slate.com]

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