Results 81 to 90 of about 102,116 (247)

Occurrence and Provenance of KREEP Components in Glassy Agglutinates From Chang'e‐5 Lunar Regolith

open access: yesGeochemistry, Geophysics, Geosystems, Volume 27, Issue 7, July 2026.
Abstract This study investigates the petrogenesis of glassy agglutinates in a polished section of the Chang'e‐5 lunar regolith sample CE5C0800YJYX018GP through integrated petrographic, mineralogical, and geochemical analyses of four representative particles (18GP‐01 to 18GP‐04).
Shuai Ma, Zhipeng Xia, Bingkui Miao
wiley   +1 more source

Use of orbiting reflectors to decrease the technological challenges of surviving the lunar night

open access: yes, 2011
In this paper the feasibility of using lunar reflectors to decrease the technological challenges of surviving the lunar night is investigated. This is achieved by attempting to find orbits in the two-body problem where the argument of periapsis is ...
Bewick, Russell   +2 more
core  

Low Abundances of Ultramafic Components in the Chang'e‐6 Landing Site Basalt and Ejecta Material

open access: yesGeophysical Research Letters, Volume 53, Issue 12, 28 June 2026.
Abstract The South Pole‐Aitken (SPA) Basin, the Moon's largest impact structure, holds key insights into lunar evolution, prompting the Chang'e‐6 mission to return first samples for ground‐truth verification. Analysis of over 6,000 grains from the Chang'e‐6 soil returned from the SPA Basin reveals a composition dominated by clinopyroxene (26.5–32.9 vol.
Zhenbing She   +20 more
wiley   +1 more source

Lunar Rover with Multiple Science Handling Capability

open access: yes, 2008
A rover design study was undertaken for exploration of the Moon. Rovers that have been launched in the past carried a suite of science payload either onboard its body or on the robotic arm’s end.
Krenn, Rainer   +3 more
core  

Evaluating the Depth–Age Hypothesis for the Evolution of the Lunar Regolith

open access: yesThe Planetary Science Journal
Lunar regolith is the fractured rock layer covering most of the lunar surface. This rock is fractured into regolith primarily by repeated meteorite impacts over eons.
Gwendolyn D. Bart
doaj   +1 more source

Regolith in Motion: Dynamic Surface Evolution After Lunar Impacts

open access: yesGeophysical Research Letters, Volume 53, Issue 12, 28 June 2026.
Abstract Multi‐temporal observations captured by the Lunar Reconnaissance Orbiter Camera provide valuable insights into contemporary surface changes. These images reveal that minor impact events (resulting in <100‐m diameter craters) significantly alter regolith structure over great distances (>1,000 crater diameters) by increasing the meter‐to ...
E. J. Speyerer   +2 more
wiley   +1 more source

Use of Silica Dust and Lunar Simulants for Assessing Lunar Regolith Exposure

open access: yes, 2023
The utilization of the lunar regolith holds immense potential for future space exploration, but the potential health risks associated with lunar regolith are a significant concern.
Irizarry-Colon, Layzamarie
core  

Sintering lunar regolith pellets: a comparison of four samples from Apollo 11, 15, and 16

open access: yesMaterials Today Advances
Lunar regolith sintering is proposed as a technique to produce consolidated objects on the lunar surface from locally sourced materials. Understanding the sintering behaviour of real lunar regolith is necessary to optimise this process, however, due to ...
Bethany A. Lomax   +7 more
doaj   +1 more source

Lunar rock investigation and tri-aspect characterization of lunar farside regolith by a digital twin

open access: yesNature Communications
Yutu-2 rover conducted an exciting expedition on the 41st lunar day to investigate a fin-shaped rock at Longji site (45.44°S, 177.56°E) by extending its locomotion margin on perilous peaks.
Liang Ding   +27 more
semanticscholar   +1 more source

Sintering Data for Lunar Regolith Simulants

open access: yes, 2023
This dataset contains raw and processed data on the sintering of Lunar regolith simulant powders by pressureless isothermal ...
Bullard, Jeff
core   +1 more source

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