Jansen, C. A.; Burkhardt, C.; Marrocchi, Y.; Schneider, J. M.; Wölfer, E.; Kleine, T.: Condensate evolution in the solar nebula inferred from combined Cr, Ti, and O isotope analyses of amoeboid olivine aggregates. Earth and Planetary Science Letters 627, p. 118567 (2024)
Jansen, C. A.; Burkhardt, C.; Marrocchi, Y.; Schneider, J.M.; Wölfer, E.; Kleine, T.: Condensate evolution in the solar nebula inferred from combined Cr, Ti, and O isotope analyses of amoeboid olivine aggregates. Earth and Planetary Science Letters 627, p. 118567 (2024)
Schneider, J.M.; Kleine, T.: Effects of Faraday cup deterioration on Sr and Cr isotope analyses by thermal ionization mass spectrometry. JOURNAL OF ANALYTICAL ATOMIC SPECTROMETRY (7), pp. 1910 - 1918 (2024)
Schneider, J. M.; Burkhardt, C.; Kleine, T.: Distribution of s-, r-, and p-process Nuclides in the Early Solar System Inferred from Sr Isotope Anomalies in Meteorites. The Astrophysical Journal 952, p. L25 (2023)
Windmill, R. J.; Franchi, I. A.; Hellmann, J. L.; Schneider, J. M.; Fridolin, S.; Kleine, T.; Greenwood, R. C.; Anand, M.: Isotopic evidence for pallasite formation by impact mixing of olivine and metal during the first 10 million years of the Solar System. PNAS Nexus 1 (1) (2022)
The dwarf planet is a bizarre, cryovolcanic world. However, the organic deposits discovered on its surface so far are unlikely to originate from its interior.
The Uranian magnetic field is more expansive than previously thought, according to newly analyzed data from Voyager 2, making it easier to search for moons with oceans.