| 词条 | Lithospheric mantle |
| 释义 |
The lithospheric mantle is the uppermost solid part of mantle. The lithospheric mantle is subdivided into the subcontinental lithospheric mantle associated with the continental lithosphere[1] and oceanic lithospheric mantle, associated with the oceanic lithosphere.[2] References1. ^{{Cite journal|jstor=3558903|title=The Continental Lithospheric Mantle: Characteristics and Significance as a mantle Reservoir|journal=Chemical reservoirs and convection in the Earth's mantle. Papers of a Discussion Meeting organized and edited by J. H. Davies|volume=360|issue=1800|pages=2383|last=|first=|date=|website=|archive-url=|archive-date=|dead-url=|access-date=|bibcode=2002RSPTA.360.2383P|author1=Pearson|first1=D. G.|last2=Nowell|first2=G. M.|year=2002|doi=10.1098/rsta.2002.1074}} {{earthsinterior}}{{geomorphology-stub}}2. ^"Oceanic lithospheric mantle beneath the continental crust of the Chinese Altai" 1 : Structure of the Earth |
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