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Lehmann discontinuity

From Wikipedia, the free encyclopedia
This article is about a discontinuity in Earth's mantle. For the discontinuity in the core, seeEarth's inner core.
Velocity of seismicS-waves in the Earth near the surface in three tectonic provinces: TNA = Tectonic North America, SNA = Shield North America and ATL = North Atlantic.[1]

TheLehmann discontinuity is an abrupt increase ofP-wave andS-wave velocities at the depth of 220 km (140 mi)[2] inEarth's mantle, discovered by seismologistInge Lehmann.[3][4][5] It appears beneathcontinents, but not usually beneathoceans,[6] and does not readily appear in globally averaged studies. Several explanations have been proposed: a lower limit to the pliableasthenosphere, aphase transition,[7] and most plausibly, depth variation in theshear waveanisotropy.[8]


Notes

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  1. ^Figure patterned afterDon L Anderson (2007).New Theory of the Earth (2nd ed.).Cambridge University Press. p. 102, Figure 8.6.ISBN 978-0-521-84959-3.; Original figure attributed to Grand and Helmberger (1984)
  2. ^Deuss, Arwen; Woodhouse, John H. (2004-09-15)."The nature of the Lehmann discontinuity from its seismological Clapeyron slopes".Earth and Planetary Science Letters.225 (3):295–304.doi:10.1016/j.epsl.2004.06.021.ISSN 0012-821X.
  3. ^William Lowrie (1997).Fundamentals of geophysics. Cambridge University Press. p. 158.ISBN 0-521-46728-4.
  4. ^Lehmann, I. (1936): P', Publications du Bureau Central Seismologique International, Série A, Travaux Scientifique, 14, 87–115.
  5. ^Martina Kölbl-Ebert (December 2001)."Inge Lehmann's paper: " P' " (1936)"(PDF).
  6. ^Lars Stixrude and Carolina Lithgow-Bertolloni (2005)."Mineralogy and elasticity of the oceanic upper mantle: Origin of the low-velocity zone".J. Geophys. Res.110 (B3): B03204.Bibcode:2005JGRB..110.3204S.doi:10.1029/2004JB002965.hdl:2027.42/94924.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.
  7. ^Kent C. Condie (1997).Plate tectonics and crustal evolution (4th ed.).Butterworth-Heinemann. p. 123.ISBN 0-7506-3386-7.
  8. ^MK Savage, KM Fischer CE Hall (2004)."Strain modelling, seismic anisotropy and coupling at strike-slip boundaries...". In John Gocott (ed.).Vertical coupling and decoupling in the lithosphere;Volume 227 of special publications.Geological Society. p. 14.ISBN 1-86239-159-9.

General references

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Further reading

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Shun-ichirō Karato (2008).Deformation of earth materials: an introduction to the rheology of solid earth. Cambridge University Press. p. 318.ISBN 978-0-521-84404-8.

External links

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Shells
Global discontinuities
Regional discontinuities


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