Abstract Details
(2020) Diamond Formation from the Lithosphere to the Lower Mantle Revealed by Koffiefontein Diamonds
Meyer NA, Stachel T, Pearson DG, Stern RA & Harris JW
https://doi.org/10.46427/gold2020.1790
The author has not provided any additional details.
03g: Room 1, Thursday 25th June 00:33 - 00:36
Nicole Anne Meyer
Thomas Stachel View all 2 abstracts at Goldschmidt2020 View abstracts at 19 conferences in series
D Graham Pearson
Richard A Stern View abstracts at 5 conferences in series
Jeffrey W Harris View abstracts at 2 conferences in series
Thomas Stachel View all 2 abstracts at Goldschmidt2020 View abstracts at 19 conferences in series
D Graham Pearson
Richard A Stern View abstracts at 5 conferences in series
Jeffrey W Harris View abstracts at 2 conferences in series
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Submitted by Jingao Liu on Saturday 20th June 20:30
Hi Nicole, Nice finding. Do you agree that around 660km it may accumulate diamonds from early magma ocean (https://www.sciencedirect.com/science/article/abs/pii/S0009254117304308)? These diamonds may be oxidized to form carbonates via decompositon of bridgmanite to release ferric iron, where kimberlite source may be derived.
Hi Nicole, Nice finding. Do you agree that around 660km it may accumulate diamonds from early magma ocean (https://www.sciencedirect.com/science/article/abs/pii/S0009254117304308)? These diamonds may be oxidized to form carbonates via decompositon of bridgmanite to release ferric iron, where kimberlite source may be derived.
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