Petrographic (optical, polarizing) microscopes open doors to the architecture of rocks – crystals, grains, cements
Category: Under the microscope
Greywacke petrography On the outside, greywacke is generally presented in varying shades of grey commonly
The selection of sandstones in plain polarized light (left) and crossed nicols (right) shown here
Absolute zero: The theoretical temperature, measured in degrees Kelvin (K), where the kinetic energy of
Pressure solution and stylolite formation in carbonates. This is part of the How To…series on
This is part of the How To…series on carbonate rocks Diagenesis of carbonate sediment begins
This is part of the How To…series on carbonate rocks Some general statements about
Early lithification of beach sand. This is part of the How To…series on carbonate
Diagenesis on the sea floor – This is part of the How To…series on carbonate
This is part of the of How To…series… on carbonate rocks The diagrams and images