Читать книгу Applied Soil Chemistry - Группа авторов - Страница 44

According to Goldich et al., in the year 1938 [31–33], stability sequence of coarsely grained minerals was reported as (most stable first) quartz, muscovite, orthoclase, plagioclase, biotite, amphibole, and pyroxene. Marel et al., in the years 1949, 1948a, and 1947 [34–36] reported magmatic minerals stability, keeping the particle size and weathering conditions similar (most resistant first), quartz, tourmaline, rutile, staurolite, zircon, allanite, albite, microcline, orthoclase, garnet, muscovite, oligodase, andesine, bytownite, epidote, anorthite, ampjibole, augite, biotite, hypersthene, olivine, and volcanic glass. As coarsely grinded quartz is not susceptible toward weathering, it is considered as stable among all the minerals.