Moho Discontinuity
The "Moho Discontinuity" is a seismological boundary surface within the Earth's interior that demarcates the base of the crust and the onset of the mantle, distinguished by an abrupt increase in seismic wave velocity due to a change in rock composition and density.
302
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16.3K
Citations
931
Authors
324
Institutions
Publications per year
2017–2026
49
Variants
MohoMohorovičić Discontinuity
Parents
302
An inverted continental Moho and serpentinization of the forearc mantle
M. G. Bostock, R. D. Hyndman, S. Rondenay et al. · Nature · 2002 · 626 citations
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GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
22 h-index
59 publications
4.6K citations

Chinese Academy of Sciences
Beijing, China
17 h-index
76 publications
4.3K citations
Institute of Geology and Geophysics
Beijing, China
15 h-index
54 publications
3.5K citations
National Geophysical Research Institute
Hyderabad, India
10 h-index
24 publications
1.2K citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
10 h-index
20 publications
808 citations
Institute of Geophysics Polish Academy of Sciences
Warsaw, Poland
8 h-index
12 publications
495 citations

Tohoku University
Sendai, Japan
8 h-index
25 publications
799 citations
The University of Tokyo
Tokyo, Japan
7 h-index
18 publications
501 citations
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GJI · 43 publications · 2.1K citations
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28 publications · 1.5K citations
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JGR · 24 publications · 2.1K citations
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20 publications · 1.2K citations
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BSSA · 16 publications · 979 citations
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