Crystal preferred orientations of olivine, orthopyroxene, serpentine, chlorite, and amphibole, and implications for seismic anisotropy in subduction zones: a review

Author:

Jung Haemyeong

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences,General Environmental Science

Reference194 articles.

1. Abramson, E.H., Brown, J.M., Slutsky, L.J., and Zaug, J., 1997, The elastic constants of San Carlos olivine to 17 GPa. Journal of Geophysical Research: Solid Earth, 102, 12253–12263.

2. Abt, D.L., Fischer, K.M., Abers, G.A., Protti, M., González, V., and Strauch, W., 2010, Constraints on upper mantle anisotropy surrounding the Cocos slab from SK(K)S splitting. Journal of Geophysical Research: Solid Earth, 115, B06316.

3. Aleksandrov, K., Alchikov, U., Belikov, B., Zaslavskii, B., and Krupnyi, A., 1974, Velocities of elastic waves in minerals at atmospheric pressure and increasing precision of elastic constants by means of EVM. Izvestiya Akademii Nauk SSSR, Seriya Geologicheskaya, 10, 15–24. (in Russian)

4. Aleksandrov, K.S. and Ryzhova, T.V., 1961a, The elastic properties of rock-forming minerals, I: pyroxenes and amphiboles. Bulletin of the Academy of Sciences of the USSR: Geophysics series, 871–875, 1339–1344.

5. Aleksandrov, K. and Ryzhova, T., 1961b, Elastic properties of rockforming minerals II: layered silicates. Bulletin of the Academy of Sciences of the USSR: Geophysics series, English translation, 12, 1165–1168.

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