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Showing 1–6 of 6 results
Advanced filters: Author: Heng-Ci Tian Clear advanced filters

  • Analyses of Chang’e-6 samples from the lunar farside reveal high water contents and low δD values, with comparisons to other lunar samples suggesting that solar-wind-implanted surface water varies with latitude and regolith maturity.

    • Honglei Lin
    • Rui Chang
    • Yong Wei
    Research
    Nature Geoscience
    Volume: 18, P: 1097-1102

  • Isotopic analysis of basalt clasts returned from the Moon by the Chang’e-5 mission indicates that the rocks were derived from a mantle source that lacked potassium, rare-earth elements and phosphorus.

    • Heng-Ci Tian
    • Hao Wang
    • Fu-Yuan Wu
    ResearchOpen Access
    Nature
    Volume: 600, P: 59-63

  • This paper determines the oxygen fugacity of the Chang’e-6 basalts from the South Pole–Aitken (SPA) basin on the farside of the Moon. The results show that the mantle beneath the farside SPA basin is more reduced than that beneath the nearside, as determined by the Apollo and Chang’e-5 basalts.

    • Huijuan Zhang
    • Wei Yang
    • Fu-Yuan Wu
    ResearchOpen Access
    Nature Communications
    Volume: 16, P: 1-8

  • Extreme Sr–Nd depletion in 2.8-billion-year-old basalt fragments from the lunar farside South Pole–Aitken basin suggests an ultra-depleted mantle source resulting from lunar magma ocean crystallization and/or later impact-related melt extraction.

    • Qin Zhou
    • Wei Yang
    • Fu-Yuan Wu
    ResearchOpen Access
    Nature
    Volume: 643, P: 371-375

  • This work estimates the eruption volume of the young Chang’e-5 lunar samples using diffusion chronology and thermodynamic simulations, and finds that there was an increase in volcanic eruption flux about 2.0 billion years ago.

    • Heng-Ci Tian
    • Chi Zhang
    • Fuyuan Wu
    ResearchOpen Access
    Nature Communications
    Volume: 14, P: 1-9