
CAS 1318-59-8
:Chlorite-group minerals
Description:
Chlorite-group minerals are a group of phyllosilicate minerals characterized by their layered structure, which consists of alternating layers of tetrahedral and octahedral sheets. These minerals typically contain magnesium, iron, and aluminum, along with hydroxyl groups, contributing to their hydrous nature. They are generally green in color, which is a result of the iron content, and exhibit a range of physical properties, including a perfect cleavage in one direction, making them easily split into thin sheets. Chlorite-group minerals are commonly found in metamorphic rocks and are often associated with other minerals such as mica and talc. They play a significant role in geological processes, including the alteration of other minerals and the formation of soils. In terms of chemical stability, chlorite is relatively resistant to weathering, although it can be transformed into other minerals under certain conditions. The CAS number 1318-59-8 specifically refers to a type of chlorite mineral, which is often studied for its implications in geology and material science.
Formula:Unspecified
Synonyms:- Chlorite-group minerals
- Chlorite (the mineral)
- Greenite
- Hydrochlorite
- Sierralite
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