2. Definition : Textures defined as the spatial relations
within and among minerals and fluids , regardless of
Scale (or) Origin.
A Common definition for ore textures refers to
volume , grain size, shape, spatial distribution
association of each mineral in the ore.
ORE TEXTURE
4. Optical mineralogy
Texture Natural arrangements of minerals
It is useful for determining the rock type.
The Crystallization sequence
Constraining pressure _temperature history
Noting weathering and their alteration
5. Isotropic Materials
Isometric refers to the optical properties of
the mineral , which are the same and their
independent of the orientation.
Example : Isotropic minerals
• Isotropic materials show the same properties
in all directions.
6. Anisotropic Materials
Anisotropic behavior when changing orientation
include different absorption of light, different
refractive indexes etc…
• All minerals , other than those belonging to
the isometric system , are anisotropic.
• Properties of material identical for depend
on the direction.
7. Optical microscopy
Light passes through thin sections _ rock cut
and polished to about 0.3 mm thickness.
Use properties of light absorption and their
propagation through a mineral _ affected by
atomic arrangement and composition.
The properties of light associated with an
techniques governing the use of a petrographic
microscope..
9. Magmatic ores
Cumulus Texture :
Settling of an ore deposit from a crystalizing magma
Example : Chromite
Intergranular (or) intercumulus Texture :
• Ore mineral occurs as an intergranular anhedral
phase relative to the other gangue mineral
• This ore mineral crystallizes Late in the magmatic
sequence , ( relative to the other gangue minerals )
10. Magmatic ores
Exsolution Texture :
• Exsolution textures usually indicate
a slow (or) intermediate cooling rate
• Exsolution textures as difficult to tell
apart from, some textures that from by replacement.