mineral
verifiedCite
While every effort has been made to follow citation style rules, there may be some discrepancies.Please refer to the appropriate style manual or other sources if you have any questions.
Select Citation Style
Feedback
Thank you for your feedback
Our editors will review what you’ve submitted and determine whether to revise the article.
verifiedCite
While every effort has been made to follow citation style rules, there may be some discrepancies.Please refer to the appropriate style manual or other sources if you have any questions.
Select Citation Style
Written and fact-checked by
The Editors of Encyclopaedia Britannica
chlorite
- Related Topics:
- chamosite
- leptochlorite
- clinochlore
- sudoite
- donbassite
chlorite, widespread group of layer silicate minerals occurring in both macroscopic and clay-grade sizes; they are hydrous aluminum silicates, usually of magnesium and iron. The name, from the Greek for “green,” refers to chlorite’s typical colour. Chlorites have a silicate layer structure similar to that in micas with compositions near (Mg,Fe,Al)3 (Si,Al)4O10(OH)2 and with brucitelike interlayers with compositions near (Mg,Fe,Al)3(OH)6. The overall composition is then (Mg,Fe,Al)6 (Si,Al)4O10(OH)8. The great many names found in older literature for chlorites with small variations of chemical composition are no longer used. The accepted names are: clinochlore (Mg-rich chlorite), chamosite (Fe-rich), nimite (Ni-rich), and pennantite (Mn-rich). Adjectival modifiers are used to indicate compositional variations. Cookeite (with lithium substituted for aluminum) is also a member of the chlorite group.
Chlorites characteristically occur as alteration products of other minerals. They are common rock-forming minerals in clastic sediments and in hydrothermally altered igneous rocks; chlorites are widespread and important constituents of such metamorphic rocks as greenschists or chlorite schists. For detailed structure and physical properties, see clay mineral (table).
This article was most recently revised and updated by John P. Rafferty.
