Solidification of Earth's mantle led inevitably to a basal magma ocean. [PDF]
Boukaré CÉ, Badro J, Samuel H.
europepmc +1 more source
Magmatic immiscibility provides phosphate for prebiotic chemistry. [PDF]
Weller D +7 more
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Apollo Next Generation Sample Analysis (ANGSA): an Apollo Participating Scientist Program to Prepare the Lunar Sample Community for Artemis. [PDF]
Shearer CK +47 more
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Metamorphism of Venus as driver of crustal thickness and recycling. [PDF]
Semprich J +4 more
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Mineralogical evidence for hydrothermal alteration of Bennu samples. [PDF]
Zega TJ +72 more
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Hydrothermal alteration of Ryugu from a disruptive impact recorded in a returned sample. [PDF]
Schrader DL +3 more
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When wet meets dry: An Ivuna-like impactor triggered volatile loss on the angrite parent body. [PDF]
Zhu 朱柯 K +5 more
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Post-Imbrium Pb-Pb isochron ages for Apollo basaltic impact melt samples 14078 and 68415. [PDF]
Snape JF +7 more
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High-energy impact and vapor recondensation history of the angrite parent body revealed by nickel isotopes. [PDF]
Zhu K +5 more
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