Mineral structures and the composition of the deep Earth
Upper mantle:
- from the Moho to 400 km:
- 54% of olivine, alpha phase
- 28% of pyroxenes: orthopyroxene (Mg,Fe)SiO3 et clinopyroxene (Ca,Mg,Fe)2Si2O6
- 18% of garnets: (Mg,Fe,Ca)3Al2Si3O12
- from 400 km to 670 km:
- 52% of wadsleyite (beta phase), and then ringwoodite (gamma phase)
- 48% of garnets
Lower mantle:
- 5% of perovskite CaSiO3
- 75% of perovskite (Mg,Fe,Al)SiO3
- 20% of magnésiowüstite (Mg,Fe)O
Inner core:
Miscaneleous:
The java animations on these pages use the freely available java applet Crystal Atomic Lattice Viewer.
Sebastien Merkel, 02/2001