Elasticity of forsterite to 16 gpa and the composition of the upper mantle
- Select a language for the TTS:
- UK English Female
- UK English Male
- US English Female
- US English Male
- Australian Female
- Australian Male
- Language selected: (auto detect) - EN
Play all audios:

ABSTRACT NEARLY 60 years ago, Bernal1 proposed that a polymorphic phase transformation in olivine might be responsible for the seismic velocity discontinuity near 410 km depth in the mantle.
Phase equilibria experiments2,3 have since shown that the olivine (α) to wadsleyite (β) transition in (Mg,Fe)2SiO4 occurs at the appropriate pressure (13.8 GPa) under mantle conditions.
Comparison of laboratory measurements of the acoustic velocity contrast in the α–β system to the magnitude of the seismically observed discontinuity at 410 km provides a way to constrain the
olivine content of the mantle at this depth. Here we report measurements of the full set of elastic moduli of single-crystal forsterite (α-Mg2SiO4) at pressures between 3 and 16 GPa, using
Brillouin scattering in a diamond anvil cell. At 13.8 GPa, the aggregate compressional-and shear-wave velocities of α-Mg2SiO4 are 2.7 ± 0.7% lower than predicted from earlier low-pressure
data4,5. From our data, and assuming a homogeneous mantle composition, the seismic velocity contrast at 410 km depth can be satisfied only by a mantle containing less than ~40% olivine. This
is well below the olivine abundance assumed in peridotite-based upper-mantle models. Access through your institution Buy or subscribe This is a preview of subscription content, access via
your institution ACCESS OPTIONS Access through your institution Subscribe to this journal Receive 51 print issues and online access $199.00 per year only $3.90 per issue Learn more Buy this
article * Purchase on SpringerLink * Instant access to full article PDF Buy now Prices may be subject to local taxes which are calculated during checkout ADDITIONAL ACCESS OPTIONS: * Log in
* Learn about institutional subscriptions * Read our FAQs * Contact customer support SIMILAR CONTENT BEING VIEWED BY OTHERS THE INFLUENCE OF Δ-(AL,FE)OOH ON SEISMIC HETEROGENEITIES IN
EARTH’S LOWER MANTLE Article Open access 08 June 2021 VARIATION IN BRIDGMANITE GRAIN SIZE ACCOUNTS FOR THE MID-MANTLE VISCOSITY JUMP Article Open access 05 July 2023 PERICLASE DEFORMS MORE
SLOWLY THAN BRIDGMANITE UNDER MANTLE CONDITIONS Article Open access 11 January 2023 REFERENCES * Bernal, J. D. _The Observatory_ 59, 268 (1936). Google Scholar * Ringwood, A. E.
_Composition and Petrology of the Earth's Mantle_ (McGraw-Hill, New York, 1975). Google Scholar * Akaogi, M., Ito, E. & Navrotsky, A. _J. geophys. Res._ 94, 15671–15685 (1989).
Article ADS Google Scholar * Kumazawa, M. & Anderson, O. L. _J. geophys. Res._ 74, 5961–5972 (1969). Article ADS CAS Google Scholar * Graham, E. K. & Barsch, G. R. _J.
geophys. Res._ 74, 5949–5959 (1969). Article ADS CAS Google Scholar * Nolet, G., Grand, S. P. & Kennett, B. L. N. _J. geophys. Res._ 99, 23753–23766 (1994). Article ADS Google
Scholar * Gwanmesia, G. D., Rigden, S., Jackson, I. & Liebermann, R. C. _Science_ 250, 794–797 (1990). Article ADS CAS Google Scholar * Weidner, D. J. _Geophys. Res. Lett._ 12,
417–420 (1985). Article ADS CAS Google Scholar * Bina, C. R. & Wood, B. J. _Nature_ 324, 449–451 (1986). Article ADS Google Scholar * Duffy, T. S. & Anderson, D. L. _J.
geophys. Res._ 94, 1895–1912 (1989). Article ADS CAS Google Scholar * Ita, J. & Stixrude, L. _J. geophys. Res._ 97, 6849–6866 (1992). Article ADS CAS Google Scholar * Isaak, D.
G., Anderson, O. L. & Goto, T. _J. geophys. Res._ 94, 5895–5906 (1989). Article ADS CAS Google Scholar * Webb, S. L. _Phys. Chem. Miner._ 16, 684–692 (1989). Article ADS CAS
Google Scholar * Isaak, D. G. _J. geophys. Res._ 97, 1871–1885 (1992). Article ADS CAS Google Scholar * Yoneda, A. & Morioka, M. in _High-Pressure Research: Applications to Earth
and Planetary Sciences_ (eds Syono. Y. & Manghnani, M. H.) 207–214 (Terra Scientific, Tokyo, 1992). Google Scholar * Fei, Y. _et al._ _J. geophys. Res._ 97, 4489–4495 (1992). Article
ADS CAS Google Scholar * Zaug, J. M., Abramson, E. H., Brown, J. M. & Slutsky, L. J. _Science_ 260, 1487–1490 (1993). Article ADS CAS Google Scholar * Meng, Y. _et al._ _J.
geophys. Res._ 98, 22199–22208 (1993). Article ADS CAS Google Scholar * Mao, H. K. & Bell, P. M. _Yb. Carnegie Instn Wash._ 79, 409–411 (1980). Google Scholar * Mao, H. K., Xu, J.
& Bell, P. M. _J. geophys. Res._ 91, 4673–4676 (1986). Article ADS CAS Google Scholar * Downs, R. T., Zha, C. S., Duffy, T. S. & Finger, L. W. _Am. Miner._ (in the press). * Zha,
C. S., Duffy, T. S., Mao, H. K. & Hemley, R. J. _Phys. Rev._ B48, 9246–9255 (1993). Article CAS Google Scholar * Every, A. G. _Phys. Rev._ B22, 1746–1760 (1980). Article ADS
MathSciNet CAS Google Scholar * Watt, J. P., Davies, G. F. & O'Connell, R. J. _Rev. Geophys. Space Phys._ 14, 541–563 (1976). Article ADS CAS Google Scholar * Davies, G. F.
& Dziewonski, A. M. _Phys. Earth planet. Inter._ 10, 336–343 (1975). Article ADS CAS Google Scholar * Sawamoto, H., Weidner, D. J., Sasaki, S. & Kumazawa, M. _Science_ 224,
749–751 (1984). Article ADS CAS Google Scholar * Grand, S. P. & Helmberger, D. V. _Geophys. J. R. astr. Soc._ 76, 399–438 (1984). Article ADS Google Scholar * Walck, M. C.
_Geophys. J. R. astr. Soc_ 76, 697–723 (1984). Article ADS Google Scholar * Mechie, J. _et al._ _Earth planet. Inter._ 79, 269–286 (1993). Article ADS Google Scholar * Sumino, Y. &
Anderson, O. L. in _Handbook of Physical Properties of Rocks_ Vol. III (ed. Carmichael, R. S.) 39–137 (CRC, Boca Raton, FL. 1989). Google Scholar * Akaogi, M. & Akimoto, S. _Phys.
Earth planet. Inter._ 19, 31–51 (1979). Article ADS CAS Google Scholar Download references AUTHOR INFORMATION Author notes * Thomas S. Duffy Present address: Consortium for Advanced
Radiation Sources, The University of Chicago, 5640 South Ellis, Chicago, Illinois, 60637, USA AUTHORS AND AFFILIATIONS * Geophysical Laboratory and Center for High-Pressure Research,
Carnegie Institution of Washington, 5251 Broad Branch Road, NW, Washington, DC, 20015, USA Thomas S. Duffy, Chang-sheng Zha, Robert T. Downs, Ho-kwang Mao & Russell J. Hemley Authors *
Thomas S. Duffy View author publications You can also search for this author inPubMed Google Scholar * Chang-sheng Zha View author publications You can also search for this author inPubMed
Google Scholar * Robert T. Downs View author publications You can also search for this author inPubMed Google Scholar * Ho-kwang Mao View author publications You can also search for this
author inPubMed Google Scholar * Russell J. Hemley View author publications You can also search for this author inPubMed Google Scholar RIGHTS AND PERMISSIONS Reprints and permissions ABOUT
THIS ARTICLE CITE THIS ARTICLE Duffy, T., Zha, Cs., Downs, R. _et al._ Elasticity of forsterite to 16 GPa and the composition of the upper mantle. _Nature_ 378, 170–173 (1995).
https://doi.org/10.1038/378170a0 Download citation * Issue Date: 09 November 1995 * DOI: https://doi.org/10.1038/378170a0 SHARE THIS ARTICLE Anyone you share the following link with will be
able to read this content: Get shareable link Sorry, a shareable link is not currently available for this article. Copy to clipboard Provided by the Springer Nature SharedIt content-sharing
initiative