Webc-axis parallel section (left) and subhedral basal section (right) of brown biotite. Note the presence of the one perfect cleavage on the c-axis parallel section and its absence on the basal section. The colourless inclusions … WebTwins in longitudinal section may resemble twins seen in plagioclase but thin sections may be stained to distinguish cordierite from the feldspars. Twins are more likely in cordierite from high grade metamorphic rocks than in medium-grade rocks. Optic Sign: Biaxial (+ or -) Rarely biaxial (+). 2V: 35-106° Mostly biaxial (-) with 2V between 40 ...
Hornblende vs Biotite under PPL and XPL - YouTube
WebIn PPL a thin section of Hornblende ranges from yellow -green to dark brown. Green varieties usually have X= light yellow green, Y=green or grey-green and Z=dark green. ... Hornblende is easly confused with biotite. … WebOne perfect cleavage. Colour and Pleochroism. Strongly colored brown, reddish brown, or brownish green in thin section; Stong pleochroism. Relief. moderately high positive … raw ruby for tumbling
Biotite - Clark Science Center
Web5. Sillimanite was named by George Thomas Bowen in 1824 in honor of Benjamin Silliman (Professor of Chemistry and Geology, Yale University, New Haven, Connecticut, USA). The minerals kyanite, adalusite and sillimanite are polymorphs of Al 2 SiO 5, each occurring under different temperature-pressure regimes and are therefore rarely found ... WebHigh relief in thin section. Color in thin section is a pale version of the hand sample color, and is often more lightly colored than spinel. ... a light pink color, a hexagonal shape. Inclusions are present. Click on the thumbnail to see a larger ppl/xpl rollover image. The garnet crystal is not a distinctive polygonal shape, however it is ... Web5. Kyanite was named in 1789 by Abraham Gottlieb Werner from the Greek word "kyanos", meaning "blue". Kyanite (also know as disthene) is a mineral, commonly found in aluminium-rich metamorphic rocks. Kyanite in metamorphic rocks generally forms at medium to high pressures and low to moderate temperatures in regional metamorphism of Barrowian type. raw rules as written