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Nature Communications|April 9, 2022
Evidence for oxygen-conserving diamond formation in redox-buffered subducted oceanic crust sampled as eclogiteSonja Aulbach, Thomas StachelJournal of Physics. Condensed Matter : an Institute of Physics Journal|August 12, 2011
Formation of diamond in the Earth's mantleThomas Stachel, Jeff W HarrisScience (New York, N.Y.)|May 10, 2022
Comment on "Discovery of davemaoite, CaSiO3-perovskite, as a mineral from the lower mantle"Michael J Walter, Simon C Kohn, D Graham Pearson, et al.Nature|January 4, 2023
Extreme redox variations in a superdeep diamond from a subducted slabFabrizio Nestola, Margo E Regier, Robert W Luth, et al.Science Advances|March 13, 2024
Dense hydrated Mg-silicates in diamond: Implications for transport of H2O into the mantleLuísa D V Carvalho, Thomas Stachel, Robert W Luth, et al.Science Advances|May 15, 2026
Sublithospheric diamond constraints on the state of deeply subducted slabsQiwei Zhang, Frank E Brenker, Suzette Timmerman, et al.Science Advances|October 15, 2025
Onset of slab mantle melting in Earth's lower mantle: Evidence from ferropericlase in superdeep diamondsPeng Ni, Steven B Shirey, Michael J Walter, et al.Nature|October 18, 2023
Sublithospheric diamond ages and the supercontinent cycleSuzette Timmerman, Thomas Stachel, Janne M Koornneef, et al.Pageof 1