Evidence for the so-called giant impact theory comes from studies of oxygen isotopes in Apollo moon samples.
“We have developed a technique that guarantees perfect separation” of oxygen isotopes from other trace gases, lead researcher Daniel Herwartz, with the University of Cologne in Germany, wrote in an email to Discovery News.
The team studied several lunar meteorites and three basalt rock samples brought back by the crews of the Apollo 11, Apollo 12 and Apollo 16 missions, which took place between 1969 and 1972.
“We also had soil samples from NASA, but this material is not ideal for determining the bulk oxygen isotopic composition of the moon, as lunar soil may be contaminated by micrometeorites and the like,” Herwartz said.
The scientists were seeking evidence of Theia, a mysterious Mars-sized object that is believed to have crashed into Earth about 4.5 billion years ago, sending a cloud of debris into space that later reformed into the moon.
Most computer models predict that between 70 percent and 90 percent of the moon is Theia, which, like most planets in the solar system, should have a unique isotopic composition. If the moon was mostly Theia, scientists believe it would have a slightly different chemical makeup than Earth.
Other models predict as little as 8 percent of the moon is Theia, with the rest of the material coming from Earth.
Based on the slightly higher concentration of oxygen isotopes in the lunar samples, the actual mix of Theia and Earth in the moon may be closer to 50-50, but that has yet to be confirmed, the researchers wrote in a paper published in this week's Science.
Meanwhile, other teams of scientists have been looking at titanium, silicon, chromium, tungsten and other chemical elements, but so far the lunar samples show no detectable differences from Earth samples.
Read more at Discovery News
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