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DTSTART:20260614T110000
DTEND:20260614T120000
SUMMARY:Snapshots of deep mantle redox reactions preserved in diamonds
DESCRIPTION:<p>Diamonds provide rare direct samples from Earth’s deep mantle, preserving tiny mineral</p><p>and fluid inclusions that record the chemical and physical conditions at depths inaccessible</p><p>by other means. These inclusions offer unique insights into mantle metasomatism, fluid</p><p>circulation, redox conditions, and the processes associated with diamond formation.</p><p>In this seminar, I will discuss how diamond-hosted inclusions can be used to investigate the</p><p>evolution of deep mantle fluids and melts beneath ancient continental cratons. I will first</p><p>introduce fluid-rich diamonds and the analytical approaches used to characterize their</p><p>microinclusions, including electron microprobe analysis, Raman spectroscopy, and laser</p><p>ablation ICP-MS. I will also present a new laser-ablation-in-water sampling method that</p><p>enables improved recovery of ablated material for trace-element and radiogenic isotope</p><p>analyses of diamond-hosted fluids.</p><p>The second part of the seminar will focus on recent work on unusual diamonds from the</p><p>Voorspoed mine (Kaapvaal craton, South Africa) that contain coexisting nickel-rich metallic</p><p>and carbonate inclusions trapped within the same growth zones. Integrated spectroscopic,</p><p>chemical, and crystallographic analyses indicate that these inclusions formed during</p><p>interaction between oxidized carbon-rich melts derived from subducted material and</p><p>reduced mantle rocks in the deep upper mantle. The observed assemblages record</p><p>transient redox reactions, redistribution of nickel between metallic and carbonate phases,</p><p>and diamond growth during metasomatism.</p><p>These observations provide rare natural evidence for redox-driven metasomatic processes</p><p>operating at depths of several hundred kilometers and demonstrate the exceptional ability</p><p>of diamonds to preserve dynamic chemical processes in Earth’s mantle. Together, the</p><p>results highlight the central role of deep mantle fluids and melts in modifying the lithosphere</p><p>and contributing to the chemical evolution of Earth’s interior.</p>
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TRANSP:OPAQUE
URL:https://www.weizmann.ac.il/EPS/events
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