[HTML][HTML] Geologic context of Chang'e-6 candidate landing regions and potential non-mare materials in the returned samples

Z Jia, J Chen, J Kong, L Qiao, X Fu, Z Ling - Icarus, 2024 - Elsevier
Our understanding of the lunar farside from orbital remote sensing is limited by the lack of
ground-truth constraints from returned samples. China's Chang'e-6 (CE-6) mission plans to …

Orbital characterization of the composition and distribution of spinels across the Crisium region: Insight from Luna 20 samples

DP Moriarty III, SB Simon, CK Shearer… - Journal of …, 2023 - Wiley Online Library
Spinels represent a small fraction of lunar surface materials but provide important insights
into the petrological evolution of the lunar crust and mantle. Previous remote sensing …

[HTML][HTML] Elemental analyses of feldspathic to basaltic soils and rocks on the moon using laser-induced breakdown spectroscopy

K Yumoto, Y Cho, JA Ogura, S Kameda… - … Acta Part B: Atomic …, 2024 - Elsevier
In-situ analysis of major elements using laser-induced breakdown spectroscopy (LIBS) is
essential for future lunar landing missions, yet its performance under lunar conditions …

Compositional diversity in the Mare Marginis and Mare Smythii: An insight into the volcanism in the region

N Panwar, N Srivastava, M Bhatt, A Bhardwaj - Icarus, 2023 - Elsevier
Abstract The Marginis-Smythii region of the eastern limb of the Moon is a unique geological
setting with the presence of equally widespread volcanism both inside and outside of an …

Spectral evidence for a pyroclastic mantle over the Tacquet formation and Menelaus domes of southwest Mare Serenitatis

WH Farrand, CS Edwards, CT Udovicic - Icarus, 2022 - Elsevier
Abstract The Tacquet Formation (TF) was first identified in geologic mapping of southern
Mare Serenitatis as a distinct low albedo region split by the linear Rimae Menelaus rilles. A …