Sericite - Wikipedia
Sericite is the name given to very fine, ragged grains and aggregates of white (colourless) micas, typically made of muscovite, illite, or paragonite. [1] Sericite is produced by the alteration of orthoclase or plagioclase feldspars in areas that have been subjected to hydrothermal alteration (also see Sericitic alteration ) typically ...
绢云母（云母的种类）_百度百科
绢云母（Sericite）是云母的一种，它属于具有层状结构的硅酸盐矿物质。 绢云母具有很广泛的用途，用于橡胶、塑料、涂料、油漆、陶瓷、保温、化妆品、颜料、造纸、冶金等行业。
Sericite | Properties, Occurrence and Uses » Geology Science
2023年4月23日 · Sericite is a type of mineral that belongs to the mica group. It is a fine-grained, muscovite mica with a silky luster and is typically white, gray, or pale yellow in color. Sericite is found in a wide range of rock types, including metamorphic, igneous, and sedimentary rocks.
sericite（英语单词）_百度百科
sericite，英语单词，主要用作名词，作名词时译为“丝（绢）云母”。 [1] Sericite is a new type of mineral filler.绢云母是一种质优价廉的矿物填料。 A detailed study is made of classification parameter, establishing the process and equipment suitable for producing multi size fraction sericite.对分级参数进行了详细的研究，获得了适合多粒级绢云母生产的工艺和设备参数。
Sericite: Mineral information, data and localities. - mindat.org
Sericite: Mineral information, data and localities. This page is currently not sponsored. Click here to sponsor this page. Named in 1852 by Karl/Carl List from the Greek seirος meaning "silken". A variety of Muscovite A term for a fine-grained white, pale green to oily greenish mica, mainly Muscovite (rarely Paragonite).
绢云母-Sericite-矿物介绍-矿物百科-石器时代 - 矿物晶体-矿物标本 …
绢云母（Sericite）是一种天然细粒白云母，属白云母的亚种，是层状结构的硅酸盐，结构由两层硅氧四面体夹着一层铝氧八面体构成的复式硅氧层。 解理完全，可劈成极薄片状，片厚可达1u以下（理论上可削成0.001u），径厚比大；与白云母相比：具有天然粒径小 ...
Sericite | mineral | Britannica
Sericite, fine-grained variety of either of the silicate minerals muscovite and paragonite
Sericite - Academic Dictionaries and Encyclopedias
Sericite is a common alteration mineral of orthoclase or plagioclase feldspars in areas that have been subjected to hydrothermal alteration typically associated with copper, tin, or en-academic.com
Sericite - Geology North
Sericite, the fine-grained form of muscovite or ‘white mica’, occurs as a result of hydrothermal alteration processes in rocks throughout the Cheviot Hills. It is commonly seen in altered feldspar crystals, particularly plagioclase, associated with secondary minerals that give host crystals a cloudy appearance.
Sericite thin section - Phyllosilicates - MicROCKScopic
Sericite is name given to very fine, ragged grains and aggregates of white mica – usually muscovite – produced by the alteration of feldspars or other minerals. Included grains of zircon or other radioactive minerals may form pale pleochroic halos in surrounding muscovite.