雷氏不連續面 (Chinese Wikipedia)

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Figure patterned after Don L Anderson. New theory of the earth 2nd. Cambridge University Press. 2007: 102, Figure 8.6. ISBN 0-521-84959-4. ; Original figure attributed to Grand & Helmberger (1984)
，參見 William Lowrie. Fundamentals of geophysics. Cambridge University Press. 1997: 158 [2013-03-13]. ISBN 0-521-46728-4. （原始内容存档于2013-10-13）.
Kent C. Condie. Plate tectonics and crustal evolution 4rth. Butterworth-Heinemann. 1997: 123. ISBN 0-7506-3386-7.
MK Savage, KM Fischer CE Hall. Strain modelling, seismic anisotropy and coupling at strike-slip boundaries.... John Gocott (编). Vertical coupling and decoupling in the lithosphere; Volume 227 of special publications. Geological Society. 2004: 14. ISBN 1-86239-159-9.

Lars Stixrude and Carolina Lithgow-Bertolloni. Mineralogy and elasticity of the oceanic upper mantle: Origin of the low-velocity zone (PDF). J Geophys. Res. 2005, 110: B03204. doi:10.1029/2004JB002965. （原始内容 (PDF)存档于2011-08-30）. The first possible explanation is that the Lehmann is not a global feature...the Lehmann is more prevalent under continents and may be absent under all or most of the oceans.

Lars Stixrude and Carolina Lithgow-Bertolloni. Mineralogy and elasticity of the oceanic upper mantle: Origin of the low-velocity zone (PDF). J Geophys. Res. 2005, 110: B03204. doi:10.1029/2004JB002965. （原始内容 (PDF)存档于2011-08-30）. The first possible explanation is that the Lehmann is not a global feature...the Lehmann is more prevalent under continents and may be absent under all or most of the oceans.

，參見 William Lowrie. Fundamentals of geophysics. Cambridge University Press. 1997: 158 [2013-03-13]. ISBN 0-521-46728-4. （原始内容存档于2013-10-13）.
Lars Stixrude and Carolina Lithgow-Bertolloni. Mineralogy and elasticity of the oceanic upper mantle: Origin of the low-velocity zone (PDF). J Geophys. Res. 2005, 110: B03204. doi:10.1029/2004JB002965. （原始内容 (PDF)存档于2011-08-30）. The first possible explanation is that the Lehmann is not a global feature...the Lehmann is more prevalent under continents and may be absent under all or most of the oceans.