Did a Giant Impact Make the Martian Moons?

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The Martian moons, Phobos and Deimos, have traditionally been thought to be captured asteroids due to their dark, cratered appearance. However, recent computer simulations suggest they may have formed from debris resulting from a significant impact on Mars, similar to the formation of Earth's moon. This alternative theory challenges the capture hypothesis, especially considering the moons' near-circular orbits aligned with Mars' equator, which complicates the capture scenario. Additionally, the spectroscopic differences between the moons and Mars, as well as their distinct characteristics compared to asteroids, raise questions about their origins. Overall, the debate continues as scientists explore various hypotheses regarding the formation of these Martian satellites.
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by Ken Croswell

The Martian moons look like asteroids—dark, crater-pocked, and potato-shaped—suggesting Mars had snatched them from the nearby asteroid belt. But now planetary scientists have conducted the first computer simulations that bolster a controversial alternative idea: The satellites formed as our own moon did, after a big object smashed into the planet and kicked up debris.

Full story: ScienceNOW
 
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CygnusX-1 said:
by Ken Croswell

The Martian moons look like asteroids—dark, crater-pocked, and potato-shaped—suggesting Mars had snatched them from the nearby asteroid belt. But now planetary scientists have conducted the first computer simulations that bolster a controversial alternative idea: The satellites formed as our own moon did, after a big object smashed into the planet and kicked up debris.

Full story: ScienceNOW
There are four different hypotheses being proposed:
  1. Phobos and Deimos were captured asteroids; or
  2. Phobos and Deimos formed during the accretion process that created Mars; or
  3. Phobos and Deimos are second-generation Solar System objects that coalesced in orbit after Mars formed, rather than forming concurrently out of the same birth cloud as Mars; or
  4. Phobos and Deimos are debris from a large impactor on Mars (similar to the Terra/Theia impact that created our moon).
The near-circular orbits of the two moons are very near to Mars' equator, which makes it difficult to reconcile in the capture theory. The problem with option #2 is that both Phobos and Deimos are spectroscopically different from Mars. Furthermore, Phobos is spectroscopically different from the asteroids in the asteroid belt. Deimos is spectroscopically similar to D-Class asteroids in the asteroid belt. If Phobos and Deimos were the debris from a large impactor on Mars, then they should both be chemically similar, but they are not. With regard to the second-generation object theory, I was not able to find a paper on the subject, just a quotation from Dr. Martin Pätzold, from the University of Cologne, Germany, and Principal Investigator of the Mars Radio Science (MaRS) experiment: http://www.esa.int/Our_Activities/Space_Science/Mars_Express/Phobos_flyby_success

See also:
Capture of Phobos and Deimos by Photoatmospheric Drag - Icarus, Volume 37, Issue 1, January 1979, Pages 113–123 (paid subscription)
http://[URL ']Formation of Phobos and Deimos via a Giant Impact[/URL] - Icarus, Volume 252, May 2015, Pages 334-338 (paid subscription) (arXiv free reprint)
 
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