0 a natural substance like glass that breaks easily into thin layers and is not damaged by heat, often used in electrical equipment
It is typically defined by the shapepreferred orientation of mica and elongated quartz grains.
Controlled deposition of lipid monolayers and bilayers onto mica and direct force measurements between galactolipid bilayers in aqueous-solutions.
The larger modelled upper continental crust component is also consistent with the relative abundance of detrital mica of possible extra-basinal origin.
The siltstones commonly contain detrital white mica flakes that are generally lacking in the sandstones, and are possibly of distal continental origin.
Low-temperature, fine-grained, alteration products include serpentine, talc, bowlingite, white mica, epidote s. l., carbonate and opaques.
Alteration is variable: absent in many crystals, in others producing dense sericite aggregates which may show some recrystallization effects to produce coarser-grained white mica.
These are mica flakes 0.5pm thick, 5-20pm diameter, coated with titanium dioxide to raise their refractive index.
The mica crystal reflectivity has not been taken into account for the calculations.
