This is a thin section of tourmaline granite from cornwall.
Tourmaline granite thin section.
Also found in metasomatically altered limestone and dolomite in contact metamorphic zones.
Fe rich chromite is typically opaque at full thin section thickness but is transparent dark brown along thin edges.
In this mode of occurrence tourmaline rarely makes up more than a few percent of the rock s volume.
This is a hydrothermally altered granite with brightly coloured xpl tourmaline some skeletal in quartz feldspar.
Tourmaline forms triangular prismatic crystals and can show a range of body colours.
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Cross polarized light photomicrograph of tourmaline in sample cv 114 from the strathbogie granite australia.
Tourmaline as an accessory mineral the most common occurrence of tourmaline is as an accessory mineral in igneous and metamorphic rocks.
It also exhibits intense pleochroism.
Tourmaline is also a common mineral in schist gneiss quartzite and phyllite.
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With chunks of feldspar scattered areas of clear and milky quartz and pieces of biotite this granite is unique in its look.
Also found as anhedral grains or irregular masses.
Longitudinal sections are usually roughly rectangular.
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Tourmaline thin section view description.
Minerals in thin section 2000 perkins dexter and henke kevin.
The thin section has been slightly rotated to show the characteristic change in color of the tourmaline known as pleochroism.
The calcium phosphate mineral apatite is a common accessory minerals of s type granites.
Acicular crystals may form radiating masses.
Every shipment will have a different structure and supply is limited.
During the polishing process an epoxy resin is applied to the surface of the stone to fill in any natural pits cracks or fissures that may exist.
Cr mg al rich chromites are realtively transparent and can be dark brown at full thin section thickness.
Tourmaline commonly forms euhedral stubby columnar to acicular crystals that show a rounded triangular or crudely hexagonal cross section.
It often occurs as millimeter size crystals scattered through granite pegmatite or gneiss.
Some relict skeletal feldspar.
In granites tourmaline is usually schorl type and it may form by late stage alteration of granitic minerals by pneumatolitic fluid containing boron and extreme tourmalinization may yield a rock of only tourmaline and quarz like luxullianite from the village of luxulyan in cornwall england.