Thin Section Granites

These are photomicrographs very thin slices of rock seen in plane polarised light or between crossed polarisers when the colours seen are produced by interference of light.

Thin section granites.

Granite ˈ ɡ r æ n ɪ t is a common type of felsic intrusive igneous rock that is granular and phaneritic in texture. Biotite metaluminous granite showing a close up of one crystal. Within the tables minerals are arranged by colour so as to help with identification. Strictly speaking granite is an.

6 1 and in the southward continuation of the slate belt in southwestern thailand comprise the western granite belt of hutchison 1973 the western tin belt granites of mitchell 1976 1977 the central and southern part of the central granitoids province of khin zaw. If a mineral commonly has a range of colours it will appear once for each colour. Enjoy the videos and music you love upload original content and share it all with friends family and the world on youtube. Identification tables for common minerals in thin section these tables provide a concise summary of the properties of a range of common minerals.

Each thin section was first scanned in unpolarized light and then again between two sheets of crossed polaroid film aligned parallel to the thin section edges. S type granites can also contain aluminium rich iron and magnesium rich biotites. The presence of these aluminous silicate minerals are commonly used as a means of initially classifying granites as s type. These are photographs of a thin section of granite magnification 10x perhaps the most common igneous rock we encounter.

By comparing the plane polarized light left and crossed polarizer right images we can see that there are three minerals in this granite. Damage produced during thin section grinding causes speckles of light in the biotite where the crystal lattice has been deformed. Quartz thin section photomicrographs are taken in plane polarized light and cross polarized light and can easily be recognized under the microscope. Rocks under the microscope.

Granites in the slate belt together with those in the shan scarps segment of the mogok metamorphic belt to the west fig. Photomicrographs of these minerals in thin section from s type granites of the lachlan fold belt are shown in figure 2a and 2b. Granites can be predominantly white pink or gray in color depending on their mineralogy the word granite comes from the latin granum a grain in reference to the coarse grained structure of such a completely crystalline rock. Biotite brown grains in plain light and pinkish brown with crossed polars the brown color is due to a property called.