Author:
Srinu Uppala,Padma Rao B.
Reference145 articles.
1. The Mg2SiO4 polymorphs (olivine, modified spinel and spinel)–thermodynamic properties from oxide melt solution calorimetry, phase relations, and models of lattice vibrations;Akaogi;Am. Mineral.,1984
2. Olivine-modified spinel-spinel transitions in the system Mg2SiO4-Fe2SiO4: Calorimetric measurements, thermochemical calculation, and geophysical application;Akaogi;J. Geophys. Res. Solid Earth,1989
3. Garnet–ilmenite–perovskite transitions in the system Mg4Si4O12–Mg3Al2Si3O12 at high pressures and high temperatures: phase equilibria, calorimetry and implications for mantle structure;Akaogi;Phys. Earth Planet. In.,2002
4. Alinaghi, A., Bock, G., Kind, R., Hanka, W., Wylegalla, K., and Tor and Svekalapko Working Groups. (2003). Receiver function analysis of the crust and upper mantle from the North German Basin to the Archaean Baltic Shield. Geophysical Journal International, 155(2), 641-652.
5. Thermally induced phase changes, lateral heterogeneity of the mantle, continental roots, and deep slab anomalies;Anderson;J. Geophys. Res. Solid Earth,1987