An example of a cross section showing gneiss, schist, sandstone... | Filo
An example of a cross section showing gneiss, schist, sandston…
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This kyanite schist thin section contains the minerals garnet, biotite, kyanite, sericite, quartz and feldspar. In the Plane Polarized view, the garnet and kyanite are grey, biotite is brown, and the sericite, quartz and feldspar are white. In the Cross Polarized view, the sericite has a distinctive bright and finely ‘speckled’ appearance. The rock has a well-developed metamorphic foliation which is most clearly defined by trails of aligned biotite crystals. Crystals of kyanite are less abundant
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Gneiss (pronounced (nice) is a foliated metamorphic rock characterized by distinct banding or layering, caused by the segregation of light- and dark-colored minerals. Appearance * Shows alternating light and dark bands * Light bands:mostly ,quartz and feldspar* * Dark bands: contain biotite, hornblende, or pyroxene * Often coarse-grained and very hard. Formation (Metamorphism) Gneiss forms through: 1. Regional metamorphism: deep burial and compression over large areas, such as mountain belts. 2.
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