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Important Non-Silicates

Important Non-Silicates

Important Non-Silicates. Hematite-Corundum. Ilmenite FeTiO 3 is similar. Halite and Galena. Pyrite. Diamond. Diamond. Sphalerite. Chalcopyrite. Halite and Calcite. Calcite. Fluorite. Uraninite UO 2 is isostructural. Goethite. Goethite. Goethite. Lepidocrocite. Lepidocrocite.

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Important Non-Silicates

Important Non-Silicates

Important Non-Silicates. Hematite-Corundum. Ilmenite FeTiO 3 is similar. Halite and Galena. Pyrite. Diamond. Diamond. Sphalerite. Chalcopyrite. Halite and Calcite. Calcite. Fluorite. Uraninite UO 2 is isostructural. Goethite. Goethite. Goethite. Lepidocrocite. Lepidocrocite.

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482 views • 30 slides
Important Non-Silicates

Important Non-Silicates

Important Non-Silicates. Hematite-Corundum. Ilmenite FeTiO 3 is similar. Halite and Galena. Pyrite. Diamond. Diamond. Sphalerite. Chalcopyrite. Halite and Calcite. Calcite. Fluorite. Uraninite UO 2 is isostructural. Goethite. Goethite. Goethite. Lepidocrocite. Lepidocrocite.

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388 views • 30 slides
Disilicates and Ring Silicates

Disilicates and Ring Silicates

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281 views • 25 slides
Crystal Field Theory; Trace Element Behavior During Melting

Crystal Field Theory; Trace Element Behavior During Melting

Crystal Field Theory; Trace Element Behavior During Melting. Lecture 25. Crystal Field Theory. Electron Orbits and Shells. Electron Shells. First Transition Metals. +2 +3 +4 +5 +6. (+2) +3 +4 +5. +3 +4. +2 +4. +2 +3. +1 +2. +3. +2. +2. +2.

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Crystal Field Theory; Trace Element Behavior During Melting

Crystal Field Theory; Trace Element Behavior During Melting

Crystal Field Theory; Trace Element Behavior During Melting. Lecture 26. Crystal Field Theory. Electron Orbits and Shells. Electron Shells. First Transition Metals. +2 +3 +4 +5 +6. (+2) +3 +4 +5. +3 +4. +2 +4. +2 +3. +1 +2. +3. +2. +2. +2.

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Weathering -II

Weathering -II

Weathering -II. THE CHEMICAL INDEX OF ALTERATION. It is predominantly feldspars that weather to clays. We can thus base a measure of the degree of weathering on how far the composition is from that of an ideal feldspar.

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Figure 1

Figure 1

Modeling Interstitial Diffusion Controlled Twinning in Alpha- Titanium Sreeramamurthy Ankem , University of Maryland, College Park, DMR 0906994.

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