Titlebook: Micromorphology of Soils; E. A. Fitzpatrick Book 1984 E.A. FitzPatrick 1984 Oxide.fabric.geomorphology.growth.microorganism.serpentine.soi

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Properties of minerals in thin sections,soil including those derived from the parent material as well as those formed in the soil. In addition the minerals are grouped according to variation in colour, pleochroism, refractive index, birefringence and maximum interference colours, and extinction angles in Tables 4.1–4.5 respectively.

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E. A. Fitzpatrickms. The interactions can involve one-photon as well as multiphoton processes in which some combinations of frequencies of participating photons are close to tran- sitions of atoms or molecules (e.g., we consider stimulated Raman scattering (SRS) as a resonant interaction). This approach involves a b

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