Metapyroxenite in the mantle transition zone revealed from majorite inclusions in diamonds
Author:
Publisher
Geological Society of America
Subject
Geology
Link
http://pubs.geoscienceworld.org/geology/article-pdf/41/8/883/3545696/883.pdf
Reference38 articles.
1. Surface waves on a spherical Earth: 1. Upper mantle structure from Love waves;Anderson;Journal of Geophysical Research,1963
2. Whole-mantle convection and the transition-zone water filter;Bercovici;Nature,2003
3. Crystal chemistry of sodium in the Earth’s interior: The structure of Na2MgSi5O12 synthesized at 17.5 GPa and 1700 °C;Bindi;American Mineralogist,2011
4. Mineral inclusions in sublithospheric diamonds from Collier 4 kimberlite pipe, Juina, Brazil: Subducted protoliths, carbonated melts and primary kimberlite magmatism;Bulanova;Contributions to Mineralogy and Petrology,2010
5. Majoritic garnet: A new approach to pressure estimation of shock events in meteorites and the encapsulation of sub-lithospheric inclusions in diamond;Collerson;Geochimica et Cosmochimica Acta,2010
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1. Cubic Fe-bearing majorite synthesized at 18–25 GPa and 1000 °C: implications for element transport, subducted slab rheology and diamond formation;Scientific Reports;2023-09-22
2. Imperfections in natural diamond: the key to understanding diamond genesis and the mantle;La Rivista del Nuovo Cimento;2023-07
3. Nature of slab-mantle interactions recorded by coupled δ13C–δ15N–δ18O signatures and elemental compositions of Koidu diamonds and their inclusions;Geochimica et Cosmochimica Acta;2023-04
4. Cubic Fe-bearing majorite synthesized at 18-25 GPa and 1000 °C: implications for element transport, subducted slab rheology and diamond formation;2023-02-15
5. Geochemistry of Silicate and Oxide Inclusions in Sublithospheric Diamonds;Reviews in Mineralogy and Geochemistry;2022-07-01
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