Transition Zone Structure
Transition Zone Structure is a seismological construct that characterizes the compositional, thermal, and mineralogical layering within the Earth's mantle between approximately 410 and 660 kilometers depth, distinguished by seismic velocity discontinuities primarily caused by phase transitions in olivine and other mantle silicates.
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Chemical Composition of Hawaiian Lavas1
Gordon A. Macdonald, Tomoo Katsura · Journal of Petrology · 1964 · 1.6K citations
Hydrous mantle transition zone indicated by ringwoodite included within diamond
D. Graham Pearson, Frank E. Brenker, Fabrizio Nestola et al. · Nature · 2014 · 788 citations · Full text
Whole-mantle convection and the transition-zone water filter
David Bercovici, Shun‐ichiro Karato · Nature · 2003 · 738 citations
Subducting slabs stagnant in the mantle transition zone
Yoshio Fukao, Masayuki Obayashi, Hiroshi Inoue et al. · Journal of Geophysical Research Atmospheres · 1992 · 667 citations
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Missouri University of Science and Technology, United States
9 publications · 561 citations
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Missouri University of Science and Technology, United States
9 publications · 561 citations
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Centre National de la Recherche Scientifique
Paris, France
22 h-index
70 publications
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Chinese Academy of Sciences
Beijing, China
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81 publications
4K citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
17 h-index
30 publications
2.4K citations
University of Cambridge
Cambridge, United Kingdom
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31 publications
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University of Bayreuth
Bayreuth, Germany
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63 publications
4.2K citations
California Institute of Technology
Pasadena, United States
14 h-index
24 publications
3K citations
Institute of Geology and Geophysics
Beijing, China
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31 publications
1.9K citations
The University of Tokyo
Tokyo, Japan
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33 publications
1.3K citations
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JGR · 62 publications · 8.2K citations
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GJI · 46 publications · 2.1K citations
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