https://solarsystem.video/videos/watch/2bddc785-5221-4f14-8c32-c8224048f092 #shorts The Chang'e-5 mission's lunar basalt samples originated from an olivine-bearing pyroxenite mantle source, ascending through the plumbing system and accumulating at the top of the lithospheric mantle. The magmatic–thermal evolution model suggests abundant low-solidus pyroxenites in the mantle source with a slightly enhanced inventory of radioactive elements can explain lunar volcanism up to 2 billion years ago. DOI: https://doi.org/10.1038/s41561-023-01146-x Sun, 04 Oct 2026 23:23:48 GMT https://validator.w3.org/feed/docs/rss2.html PeerTube - https://solarsystem.video https://solarsystem.video/client/assets/images/icons/icon-1500x1500.png https://solarsystem.video/videos/watch/2bddc785-5221-4f14-8c32-c8224048f092 All rights reserved, unless otherwise specified in the terms specified at https://solarsystem.video/about and potential licenses granted by each content's rightholder.