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jost s engineering company limited (505750) hits 52 week high ✌️【Asset Manager】✌️ Free stock selection service with professional advisors offering the best investment portfolio for stable growth. Scientists have published the first detailed analyses of the historic cache of lunar soil and rock that China retrieved from the far side of the moon this year.

Chang’e-6, the first mission to bring back soil from the moon’s far side, collected 1.9 kilograms (4.2 pounds) of lunar soil via a robotic probe in June before returning to Earth, a scientific tour de force that cemented China’s place as one of the world’s top space powers.

Volcanic rock contained in the sample dates back 2.8 billion years, suggesting the uncrewed mission’s landing site was volcanically active at that time, according to two papers published Friday in the journalsScienceandNature. The eruption represented a relatively recent episode of lunar volcanic activity not known from the study of samples taken from the moon’s near side by NASA’s Apollo program and Russia’s Luna missions, the new research found.

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“The relatively young age of the basalts (retrieved by Chang’e-6) is surprising along with the composition being practically devoid of radioactive elements,” Neal said via email. This “prompts the question ‘how and why were these magmas generated.’”

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“One of the concerns, you know, we developed this detailed story (about the moon) from all the Apollo results,” said Richard W. Carlson, staff scientist emeritus at the Carnegie Institution for Science’s Earth & Planets Laboratory in Washington, DC. He was not involved in the new research.

“And one thing that has always kind of lingered in the back of my mind is whether that only applies to the Apollo area of the moon,” Carlson added.

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Earlier research based on remote sensing revealed that the moon’s far side has different topography, a thicker crust, a different distribution of basalt as well as different concentrations of thorium, a radioactive element found in rock, Li said.

“The asymmetry between the Moon’s nearside and farside remains an unresolved mystery,” he said in an email.

Li and his team studied 108 basalt fragments contained in two small samples of the lunar far side soil. Most of the fragments formed around 2.8 billion years ago, the researchers found by studying the decay of lead isotopes in the samples.However, one fragment formed around 4.2 billion years ago, according to the research.

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“We don’t really have a good idea of why the Moon is molten that long,” Carlson said in an email. “The moon’s a pretty small body, and it should have cooled off pretty quickly.”

Both papers noted that the samples were not rich in KREEP, an acronym that stands for potassium (chemical symbol K), rare-earth elements (REE) and phosphorus (P) that has been found in other Apollo-era lunar samples.

KREEP is heat generating, Carlson said, and its existence would explain why volcanism continued on the moon for so long. He said it is interesting that the Chang’e-6 samples were devoid of the radioactive elements.

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Li said that foreign researchers such as Neal are already able to collaborate with their Chinese counterparts as part of a team.

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“The agency is aware that as part of the application process CNSA interviewed the international loan applicants but has not announced selections,” NASA said.

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