The Different of Gemstone Mineral in Chemistry Version

in #science5 years ago (edited)


Minerals in Nature

Based on chemical compounds, the minerals can be grouped into Silicate minerals and Non-silicate minerals. There are eight of non-silicate minerals group, namely Oxide, Sulfide, Sulfate, Native element, Halide, Carbonate, Hydroxide, and Phosphate (see Table B ).

The silicate minerals (containing elements of SiO) commonly found in rocks are as shown in Table A. As we know that no less than 2,000 types of minerals are known until now. However, only a few species are involved in the formation of rocks. These minerals are called Rock forming minerals, which main constituents of rocks from the Earth's crust and mantle. Rock forming minerals are group:

  1. Silicate,
  2. Oxides,
  3. Sulfides and
  4. Carbonate and Sulfate.

Silicate Mineral

Nearly 90% of rock forming minerals are from this group, which is a compound between silicon and oxygen with some metal elements. Because it has large amount, almost 90% of the Earth's crust is made up from silicate minerals, and nearly 100% of Earth's mantle (up to 2,900 km of Earth's crust). Silicates are the main parts of make up rocks, whether sediments, igneous rocks or rocks. The common rock-forming silicate is divided into two groups, namely the ferro magnesium and non-ferro magnesium groups. The Silicate mineral namely :

  1. Quartz: (SiO2)
  2. Feldspar Alkali: (KAlSi3O8)
  3. Feldspar Plagioclase: (Ca, Na) AlSi3O8)
  4. Mica Muscovite: (K2Al4(Si6Al2O20)(OH, F)2
  5. Mica Biotite: K2 (Mg, Fe) 6Si3O10(OH)2
  6. Amphibole: (Na, Ca)2(Mg, Fe, Al)3(Si, Al)8O22(OH)
  7. Pyroxene: (Mg, Fe, Ca, Na) (Mg, Fe, Al)Si2O6
  8. Olivin: (Mg, Fe)2SiO4

Note :

1 - 4 is non-ferro magnesium minerals
5 - 8 is ferro magnesium minerals

Mineral
Formula
Olivine(Mg, Fe)2SiO4
Pyroxene(Mg, Fe)SiO3
Amphibole(Ca2Mg5)Si8O22(OH)2
Mica MuscoviteK Al3Si3O10(OH)2
Mica BiotiteK(Mg,Fe)3Si3O10(OH)2
Feldspar OrthoclaseK Al Si3O8
Feldspar Plagioclase(Ca, Na)AlSi3O8
QuartzSiO3

Ferro Magnesium

Generally has a dark or black color and large density.

Olivine: known for its olive color. Specific gravity ranges from 3.27 to 3.37, growing as a mineral that has a less than perfect split area.

Augitite: the color is very dark green to black. BD ranges from 3.2 to 3.4 with the intersecting plane intersecting almost perpendicularly. This split field is very important to distinguish it from hornblende minerals.

Hornblende: the color is green to black; BD. 3.2 and having a split plane intersecting at an angle of approximately 56 ° and 124 ° which is helpful in recognizing it.

Biotite: is a flat-shaped mica mineral that can easily be exfoliated. In a thick, dark green to brown-black; BD 2.8 - 3.2.

Mineral Non Ferro Magnesium

Muscovite: Called white mica because of its bright color, light yellow, brown, green or red. BD. Ranged from 2.8 - 3.1.

Feldspar: Is the most rock-forming mineral. Its name also reflects this mineral found in every field. Feld in German is field (Field). The amount in the Earth's crust is almost 54%. The names given to feldspar are plagioclase and orthoclase. Plagioclase can then also be divided into two, albite and anorthite. Orthoclase are those containing potassium, albite containing Sodium and Anorthite containing Calcium. Orthoclase: have a distinctive color that is white gray or pink. BD. 2.57.

Table B : Non Silicate Mineral

Group
Name
Formula
OxideHematiteFe2O3
____CorundumAl2O3
____MagnetiteFe3O4
SulfidePyriteFeS2
____BorniteCu5FeS4
____CannabarHgS
SulfateGypsumCaSO4.2H2O
____AnhydriteCaSO4
____BariteBaSO4
Native ElementsGoldAu
____CoperCu
____DiamondC
HalidesHaliteNaCl
____FlouriteCaF2
____SylviteKCl
carbonateDolomiteCaMg(CO3)2
____MalachiteCu2OH2CO3

Quartz: Sometimes called silica. Its only rock-forming mineral consisting of silicon and oxygen compounds. Generally comes with colors like smoke or smooky, also called smooky quartz. Sometimes it could be purple color or red-violet (violet). Such quartz names are called amethyst, red massif or pink, yellow to brown. Various colors are caused by other elements that are not clean.

Mineral oxide.

Formed as a result of a direct compound between oxygen and certain elements. The arrangement is simpler than silicate. Mineral oxides are generally harder than other minerals except silicates. They are also heavier except sulphide. The most important ingredients in the oxides are iron, chroom, manganese, tin and aluminum. Some of the most common oxide minerals are ice (H2O), corundum (Al2O3), hematite (Fe2O3) and cassiterite (SnO2).

Mineral Sulfide.

It is a direct mineral compound of certain elements with sulfur (sulfur), such as iron, silver, copper, lead, zinc and mercury. Some of these sulphide minerals are present as materials having economic value, or ore, such as pyrite (FeS3), chalcocite (Cu2S), galena (PbS), and sphalerite (ZnS).

Carbonate and Sulfate Minerals.

Is a compound with ions (CO3)2-, and is called carbonate, for example compounds with Ca are called calcium carbonate, CaCO3 is known as calcite minerals. This mineral is the main structure that forms the sedimentary rock.


Conclusion


The strength of a gemstone power or scale of mosh is measured by compound of Oxygen molecules binding on Silica, the more Siloxane cluster (SiXOY)in a component the more high of the mosh scale.

Source

Materials Science
Minerals
Gemstone
Inorganic Chemistry


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