Ground-penetrating radar measurements taken by China's first lunar rover Yutu, also known as Jade Rabbit, found at least nine subsurface layers beneath its landing site, indicating that multiple geologic processes have taken place there.
"We have for the first time detected multiple subsurface layers (on the Moon)," said lead author Xiao Long, professor of the China University of Geosciences in Wuhan, attributing these layers to ancient lava flows and the weathering of rocks and boulders into regolith, or loose layers of dust, over the past 3.3 billion years or so.
"We think this layer is probably pyroclastic rocks which formed during the course of volcanic eruptions," Xiao told Xinhua via email.
"It reveals the diversity of volcanic activity, but what's more important is that it shows there are plenty of volatile contents inside the moon."
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Yutu is part of China's Chang'e-3 moon mission, which delivered the rover and a stationary lander to the lunar surface on December 14, 2013, marking the first moon landing since the Soviet Union's Luna 24 mission in 1976.
Yutu traveled a total of 114 metres following a zigzagging route, then came to a halt about 20 meters to the southwest of the landing site due to mechanical problems.
So the rover just surveyed a small area using two radar antennas capable of penetrating the Moon's crust to depths of about 400 metres, the report said.
The data, however, were enough to show its landing site is compositionally distinct from previous Moon-landing sites, the researchers said.
"But if we want to have a comprehensive understanding of moon's geological structure, material composition and formation, as well as its evolution, a large number of exploration events are still needed. Meanwhile, effective international cooperation is a must considering the high cost of these activities."
The findings were published in the US journal Science.