Discontinuité de Lehmann (French Wikipedia)

Analysis of information sources in references of the Wikipedia article "Discontinuité de Lehmann" in French language version.

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(en) Don L. Anderson, New Theory of the Earth, Cambridge University Press, 2007, 2^e éd., 400 p. (ISBN 978-0-521-84959-3 et 0-521-84959-4, lire en ligne), p. 102, Fig. 8.6.
(en) William Lowrie, Fundamentals of Geophysics, Cambridge, G. B., Cambridge University Press, 1997, 354 p. (ISBN 0-521-46728-4, lire en ligne), p. 158.
(en) Kent C. Condie, Plate tectonics and crustal evolution, Oxford, Butterworth-Heinemann, 1997, 4^e éd., 282 p. (ISBN 0-7506-3386-7, lire en ligne), p. 123.
(en) M. K. Savage, K. M. Fischer et C. E. Hall, « Strain modelling, seismic anisotropy and coupling at strike-slip boundaries », dans John Gocott, Vertical coupling and decoupling in the lithosphere, vol. 227, Geological Society, coll. « Special publications », 2004 (ISBN 1-86239-159-9, lire en ligne), p. 14.

(en) Lars Stixrude et Carolina Lithgow-Bertolloni, « Mineralogy and elasticity of the oceanic upper mantle : Origin of the low-velocity zone », Journal of Geophysical Research, vol. 110,‎ 2005, B03204 (DOI 10.1029/2004JB002965, lire en ligne) : «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 ».

(en) Shun-Ichiro Karato, On the Lehmann discontinuity, The Smithsonian - NASA Astrophysics Data System (1992).

(en) Lars Stixrude et Carolina Lithgow-Bertolloni, « Mineralogy and elasticity of the oceanic upper mantle : Origin of the low-velocity zone », Journal of Geophysical Research, vol. 110,‎ 2005, B03204 (DOI 10.1029/2004JB002965, lire en ligne) : «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 ».