Samples collected by Chang’e-5 are revealing exciting insights into the Moon’s evolution.
The results confirmed that the Moon was still volcanically active almost a billion years later than the rocks from Apollo suggested this activity peaked. But working out what fuelled this activity has proved tricky.
“This is a very big science problem,” says Weibiao Hsu, a planetarygeochemist at Purple Mountain Observatory, CAS, in Nanjing, China, because it reveals how much we still have to learn about the Moon’s evolution. “We’re exploring all possibilities,” says Ming Tang, a geochemist at Peking University in Beijing, who received two tiny grains of basaltic rock and will analyse them to better understand the pressure and temperature in which they were created. The samples are a first for Tang, who previously studied magma from volcanoes on Earth. “It’s a good opportunity for me and many other Chinese scientists interested in stretching their field,” says Tang.
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