Depressed 660-km discontinuity caused by akimotoite–bridgmanite transition
Depressed 660-km discontinuity caused by akimotoite–bridgmanite transition
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Publisher
London: Nature Publishing Group UK
Journal title
Language
English
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Publication information
Publisher
London: Nature Publishing Group UK
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Scope and Contents
Contents
The 660-kilometre seismic discontinuity is the boundary between the Earth’s lower mantle and transition zone and is commonly interpreted as being due to the dissociation of ringwoodite to bridgmanite plus ferropericlase (post-spinel transition)
1
–
3
. A distinct feature of the 660-kilometre discontinuity is its depression to 750 kilome...
Alternative Titles
Full title
Depressed 660-km discontinuity caused by akimotoite–bridgmanite transition
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Primary Identifiers
Record Identifier
TN_cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_8732283
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_8732283
Other Identifiers
ISSN
0028-0836
E-ISSN
1476-4687
DOI
10.1038/s41586-021-04157-z
