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Metapyroxenite in the mantle transition zone revealed from majorite inclusions in diamonds

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Authors

Kiseeva, Ekaterina
Yaxley, Gregory
Stepanov, Aleksandr
Tkalčić, Hrvoje
Litasov, Konstantin D.
Kamenetsky, Vadim S.

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Geological Society of America Inc

Abstract

The transition zone of the Earth's mantle (the depth interval between two major seismic discontinuities at 410 km and 660 km) is critical to understanding our planet's evolution. Some diamonds are thought to have originated in the transition zone and the

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Geology

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Restricted until

2037-12-31
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