| 词条 | List of mineral tests |
| 释义 |
}} Mineral tests are several methods which can help identify the mineral type. This is used widely in mineralogy, hydrocarbon exploration and general mapping. There are over 4000 types of minerals known with each one with different sub-classes. Elements make minerals and minerals make rocks so actually testing minerals in the lab and in the field is essential to understand the history of the rock which aids data, zonation, metamorphic history, processes involved and other minerals. The following tests are used on hand specimens and thin sections through polarizing microscope.
Color of the mineral. This is not mineral specific. For example quartz can be almost any color, shape and within many rock types.
Color of the mineral's powder. This can be found by rubbing the mineral onto a concrete. This is more accurate but not always mineral specific.
This is the way light reflects from the mineral's surface. A mineral can be metallic (shiny) or non-metallic (not shiny).
The way light travels through minerals. The mineral can be transparent (clear), translucent (cloudy) or opaque (none).
Ratio between the weight of the mineral relative to an equal volume of water.
The shape of the crystal and habitat.
Magnetic or nonmagnetic. Can be tested by using a magnet or a compass. This does not apply to all ion minerals (for example, pyrite).
Number, behaviour, size and way cracks fracture in the mineral.
Many minerals glow when put under a UV light.
Is the mineral radioactive or non-radioactive? This is measured by a Geiger counter.
This is not recommended. Is the mineral salty, bitter or does it have no taste?
This is recommended. This involves biting a mineral to see if its generally soft or hard. This was used in early gold exploration to tell the difference between pyrite (fools gold, hard) and gold (soft).
The Mohs Hardness Scale is the main scale to measure mineral hardness. Finger nail is 2.5, copper coin is 3.5, glass is 5.5 and steel is 6.5. Hardness scale is Talc is 1, Gypsum is 2, Calcite is 3, Fluorite is 4, Apatite is 5, Orthoclase Feldspar is 6, Quartz is 7, Topaz is 8, Corundum is 9 and Diamond is 10.
Not always recommended. Does the mineral have an odor of oil, sulfur or something else or is there no odour?
Every mineral has a different electrical resistance which is done by passing an electric current through the mineral which is received by a receiver.
Shape and structure of mineral.
Type of fracture and fracture pattern.
Mineral shape or crystal system (cubic, tetragonal, hexagonal, trigonal, orthorhombic, monoclinic or triclinic)
Colour of minerals in crossed polarized light (XPL), colour strength.
Crystal twinning present and type.
Degrees which mineral turns black in XPL in microscope.
Mineral zoning present.
Porphyritic (large xenocryst surrounded by fine crystals), Melange (mix of minerals), Poikilitic (one mineral grown around another),Polymorph (same composition but different shape), Hetrogenous (many types of minerals), Homogenous (one mineral type).
Is the mineral reactive or nonreactive? If it is reactive it usually has calcium carbonate composition.
What rock type is the mineral usually associated.
Mineral shape, properties or form been altered.
References
External links
2 : Crystallography|Mineralogy |
| 随便看 |
|
开放百科全书收录14589846条英语、德语、日语等多语种百科知识，基本涵盖了大多数领域的百科知识，是一部内容自由、开放的电子版国际百科全书。