Amphibolite, light micrograph
Polarised light micrograph of a specimen of amphibolite from a scree of the Messner-Brook, St Nikolaus, Ultental, South Tyrol, Italy. Amphibolite is composed mainly of amphibole and plagioclase feldspar (bright), with little or no quartz. It is dense with a weakly foliated or schistose (flaky) structure. This rock was formed by metamorphic transformation of basalt and gabbro at great depths and temperatures of 550-700 degrees Celsius and pressures of 200-1200 megapascals. These conditions are known as amphibolite facies. The metamorphic transformation occurred around 335 million years ago (Variscan orogeny). Magnification: x4 when printed 15 centimetres wide.
Size: 6016px × 4016px
Location:
Photo credit: © EYE OF SCIENCE/SCIENCE PHOTO LIBRARY / Alamy / Afripics
License: Licensed
Model Released: No
Keywords: -, amphibole, amphibolite, biotite, chlorite, epidote, facies, flaky, foliated, garnet, geological, geology, light, lm, metamorphic, micrograph, microscopy, mineral, mineralogical, mineralogy, petrography, plagioclase, polarised, polarized, ribbon, rock, schistose, section, south, stone, thin, tyrol, weakly
