期刊
ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES
卷 37, 期 -, 页码 19-46出版社
ANNUAL REVIEWS
DOI: 10.1146/annurev.earth.36.031207.124224
关键词
subduction; mantle dynamics; tomography; mantle discontinuity
资金
- Ministry of Education, Culture, Sports, Science, and Technology Japan
A stagnant slab is a subducted slab of oceanic lithosphere subhorizontally deflected above, across, or below the 660 km discontinuity. This phenomenon has now been widek, recognized beneath subduction zones around the circum-Pacific and in the Mediterranean. Collaboration of seismic and electromagnetic observations, mineral physics measurements, and geodynamic modeling has begun to provide a consistent picture of stagnant slab.
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