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- Epidote - Wikipedia
Epidote is an abundant rock-forming mineral, but one of secondary origin It occurs in marble and schistose rocks of metamorphic origin It is also a product of hydrothermal alteration of various minerals (feldspars, micas, pyroxenes, amphiboles, garnets, and others) composing igneous rocks
- Epidote: A metamorphic mineral and silicate mineral group.
Epidote is the word used for a calcium-iron silicate mineral that forms through regional and contact metamorphism It is also the name of a diverse group of silicate minerals that often contain rare earth elements
- Epidote Meanings and Crystal Properties - The Crystal Council
Epidote is an aluminum-iron mineral that can be found in either crystal or stone form The stone was first described in 1801 by R J Hauy and was named after the Greek word meaning to “increase” They are commonly found in Norway, U S A, and Brazil, which has been known to have the nicest crystallized forms of Epidote ever seen
- Epidote: Mineral information, data and localities. - mindat. org
Epidote Group > Epidote Supergroup Name: Named in 1801 by Rene Just Haüy from the Greek επιδοσιζ ("epidosis"), meaning "increase", in allusion to the crystal characteristic of one longer side at the base of the prism
- Epidote Group Minerals | Properties, Occurrence, Uses » Gemstone
Epidote is a mineral that belongs to the sorosilicate group and is known for its distinct green to yellow-green color It is widely found in metamorphic rocks, igneous rocks, and hydrothermal veins
- Epidote: Properties, Occurrence, Uses – Geology In
Epidote is a mineral belonging to the sorosilicate group, primarily composed of calcium, aluminum, iron, and silica It typically occurs in metamorphic rocks, where it forms as a result of the alteration of primary minerals under high-pressure and temperature conditions
- Epidote | Definition, Formula, Uses, Facts | Britannica
epidote, any of a group of colourless to green or yellow-green silicate minerals with the general chemical formula A2B3 (SiO 4) (Si 2 O 7)O (OH), in which A is usually calcium (Ca), though manganese (Mn) or cerium (Ce) is sometimes substituted, and B is generally aluminum (Al), with the main substitution being ferric iron (Fe +3)
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