PARASIBIRSKITE Meaning and
Definition
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Parasibirskite is a rare mineral that belongs to the oxide mineral group. It is typically found in hydrothermal veins associated with tin and tungsten deposits. The mineral has a distinctive yellow to orange-yellow color and exhibits a vitreous to greasy luster when observed in its natural form.
Chemically, parasibirskite is composed of the chemical elements titanium (Ti), oxygen (O), and fluorine (F). Its chemical formula is typically represented as TiO2F2. This composition places parasibirskite within the titanium dioxide mineral family, more specifically, the rutile group.
The crystal structure of parasibirskite is tetragonal, meaning it possesses four axes of equal length, two of which are perpendicular to each other. This results in the mineral having prismatic or tabular crystal habits. It has a Mohs hardness of around 6, indicating a moderate degree of hardness.
Due to its rarity and limited occurrence, parasibirskite does not have significant economic importance. However, it is of interest to mineral collectors and researchers studying mineralogy and ore deposits. Its distinct color and crystal habit contribute to its value as a unique addition to mineral collections.
Overall, parasibirskite can be defined as a rare oxide mineral composed of titanium, oxygen, and fluorine. It exhibits a tetragonal crystal structure, yellow to orange-yellow color, and is found in association with tin and tungsten deposits.
Etymology of PARASIBIRSKITE
The word "parasibirskite" is derived from its chemical composition and its geographic origin.
The prefix "para-" signifies that it is a variation or a secondary form of a similar mineral known as "sibirskite". "Sibirskite" is a mineral named after its discovery in the region of Siberia, Russia.
The suffix "-ite" is commonly used in mineralogy to denote minerals. It comes from the Greek suffix "-ites", which means "connected with" or "pertaining to".
Combining "para-" and "-sibirskite" results in the word "parasibirskite", denoting a mineral that is related or similar to the original sibirskite mineral found in Siberia.
